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	<title>Konkresi (geologi) - Riwayat revisi</title>
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	<updated>2026-09-16T08:36:52Z</updated>
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		<title>Maintenance script: Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi</title>
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		<updated>2026-08-28T03:58:32Z</updated>

		<summary type="html">&lt;p&gt;Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Revisi sebelumnya&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revisi per 28 Agustus 2026 03.58&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Baris 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Baris 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:Bowling_Balls_Beach_2_edit.jpg|thumb|right|280px|Konkresi-Konkresi bongkah yang terlapukkan dari Batugamping berumur kenozoikum, california, Amerika Serikat]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Konkresi&amp;#039;&amp;#039;&amp;#039; adalah massa kompak yang keras, terbentuk dari presipitasi semen [[mineral]] di dalam rongga-rongga partikel, dan ditemukan di [[batuan sedimen]] atau [[tanah]]. Konkresi berbentuk seperti [[telur]] ataupun bulat, tetapi bentuk-bentuk iregular juga sering terjadi. Istilah &amp;#039;konkresi&amp;#039; berasal dari [[bahasa latin]] &amp;#039;&amp;#039;Con &amp;#039;&amp;#039;yang artinya &amp;#039;bersama&amp;#039; dan &amp;#039;&amp;#039;crescere &amp;#039;&amp;#039;yang artinya &amp;#039;tumbuh&amp;#039;. Konkresi-konkresi terbentuk di perlapisan strata sedimen yang telah terendapkan terlebih dahulu. Mereka biasanya terbentuk lebih awal ketika terjadi penumpukkan sedimen, sebelum kemudian sedimen tersebut mengeras menjadi [[batu]]an. Semen konkresi ini sering menyebabkan konkresi lebih keras dan lebih tahan terhadap pelapukan dibanding perlapisan induknya.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Konkresi&amp;#039;&amp;#039;&amp;#039; adalah massa kompak yang keras, terbentuk dari presipitasi semen [[mineral]] di dalam rongga-rongga partikel, dan ditemukan di [[batuan sedimen]] atau [[tanah]]. Konkresi berbentuk seperti [[telur]] ataupun bulat, tetapi bentuk-bentuk iregular juga sering terjadi. Istilah &amp;#039;konkresi&amp;#039; berasal dari [[bahasa latin]] &amp;#039;&amp;#039;Con &amp;#039;&amp;#039;yang artinya &amp;#039;bersama&amp;#039; dan &amp;#039;&amp;#039;crescere &amp;#039;&amp;#039;yang artinya &amp;#039;tumbuh&amp;#039;. Konkresi-konkresi terbentuk di perlapisan strata sedimen yang telah terendapkan terlebih dahulu. Mereka biasanya terbentuk lebih awal ketika terjadi penumpukkan sedimen, sebelum kemudian sedimen tersebut mengeras menjadi [[batu]]an. Semen konkresi ini sering menyebabkan konkresi lebih keras dan lebih tahan terhadap pelapukan dibanding perlapisan induknya.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l6&quot;&gt;Baris 6:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Baris 8:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Galeri ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Galeri ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Sitasi ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Sitasi ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;== Referensi ==&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Al-Agha, M.R., S.D. Burley, C.D. Curtis, and J. Esson, 1995, &#039;&#039;Complex cementation textures and authigenic mineral assemblages in Recent concretions from the Lincolnshire Wash (east coast, UK) driven by Fe(0) Fe(II) oxidation&#039;&#039;: Journal of the Geological Society, London, v. 152, pp.&amp;amp;nbsp;157–171.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Boles, J.R., C.A. Landis, and P. Dale, 1985, [http://jsedres.sepmonline.org/cgi/content/abstract/55/3/398 &#039;&#039;The Moeraki Boulders; anatomy of some septarian concretions&#039;&#039;]:, Journal of Sedimentary Petrology. v. 55, n. 3, pp.&amp;amp;nbsp;398–406.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Chan, M.A. and W.T. Parry, 2002, [http://geology.utah.gov/online/pdf/pi-77.pdf &#039;&#039;&#039;Mysteries of Sandstone Colors and Concretions in Colorado Plateau Canyon Country&#039;&#039; PDF version, 468 KB] : Utah Geological Survey Public Information Series. n. 77, pp.&amp;amp;nbsp;1–19.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Chan, M.A., B.B. Beitler, W.T. Parry, J. Ormo, and G. Komatsu, 2005. [ftp://rock.geosociety.org/pub/GSAToday/gt0508.pdf &#039;&#039;Red Rock and Red Planet Diagenesis: Comparison of Earth and Mars Concretions&#039;&#039; PDF version, 3.4 MB] : GSA Today, v. 15, n. 8, pp.&amp;amp;nbsp;4–10.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Davis, J.M., 1999, &#039;&#039;Oriented carbonate concretions in a paleoaquifer: Insights into geologic controls on fluid flow&#039;&#039;: Water Resources Research, v. 35, p.&amp;amp;nbsp;1705-1712.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Hattin, D.E., 1982, &#039;&#039;Stratigraphy and depositional environment of the Smoky Hill Chalk Member, Niobrara Chalk (Upper Cretaceous) of the type area, western Kansas&#039;&#039;: Kansas Geological Survey Bulletin 225:1-108.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Hobbs, D., and J. Hafnaer, 1999, &#039;&#039;Magnetism and magneto-structural effects in transition-metal sulphides&#039;&#039;: Journal of Physics: Condensed Matter, v. 11, pp.&amp;amp;nbsp;8197–8222.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Hoffmann, V., H. Stanjek, and E. Murad, 1993, &#039;&#039;Mineralogical, magnetic and mössbauer data of symthite (Fe9S11) &#039;&#039;: Studia Geophysica et Geodaetica, v. 37, pp.&amp;amp;nbsp;366–381.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Johnson, M.R., 1989, &#039;&#039;Paleogeographic significance of oriented calcareous concretions in the Triassic Katberg Formation, South Africa&#039;&#039;: Journal of Sedimentary Petrology, v. 59, p.&amp;amp;nbsp;1008-1010.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Loope D.B., Kettler R.M., Weber K.A., 2011, &#039;&#039;Morphologic Clues to the origin of Iron Oxide-Cemented Sphereoids, Boxworks, and Pipelike Concretions, Navajo Sandstone of South-Central Utah, U.S.A,&#039;&#039; The Journal of Geology, Vol. 119, No. 5 (September 2011), pp.&amp;amp;nbsp;505–520&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Loope D.B., Kettler R.M., Weber K.A., 2011, &#039;&#039;Follow the water: Connecting a CO2 reservoir and bleached sandstone to iron-rich concretions in the Navajo Sandstone of south-central Utah, USA,&#039;&#039; GEOLOGY FORUM, November 2011, Geological Society of America doi:10.1130/G32550Y.1&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* McBride, E.F., M.D. Picard, and R.L. Folk, 1994, &#039;&#039;Oriented concretions, Ionian Coast, Italy: evidence of groundwater flow direction&#039;&#039;: Journal of Sedimentary Research, v. 64, p.&amp;amp;nbsp;535-540.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* McBride, E.F., M.D. Picard, and K.L. Milliken, 2003, [http://jsedres.sepmonline.org/cgi/content/abstract/73/3/462 &#039;&#039;Calcite-Cemented Concretions in Cretaceous Sandstone, Wyoming and Utah, U.S.A.&#039;&#039;]: Journal of Sedimentary Research. v. 73, n. 3, p.&amp;amp;nbsp;462-483.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Mozley, P.S., 1996, &#039;&#039;The internal structure of carbonate concretions: A critical evaluation of the concentric model of concretion growth: Sedimentary Geology&#039;&#039;: v. 103, p.&amp;amp;nbsp;85-91.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Mozley, P.S., and Goodwin, L., 1995, &#039;&#039;Patterns of cementation along a Cenozoic normal fault: A record of paleoflow orientations: Geology&#039;&#039;: v. 23, p 539-542.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Mozley, P.S., and Burns, S.J., 1993, &#039;&#039;Oxygen and carbon isotopic composition of marine carbonate concretions: an overview: Journal of Sedimentary Petrology, v. 63, p. 73-83.&#039;&#039;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Mozley, P.S., and Davis, J.M., 2005, &#039;&#039;Internal structure and mode of growth of elongate calcite concretions: Evidence for small-scale microbially induced, chemical heterogeneity in groundwater&#039;&#039;: Geological Society of America Bulletin, v. 117, 1400-1412.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Pratt, B.R., 2001, &quot;Septarian concretions: internal cracking caused by synsedimentary earthquakes&quot;: Sedimentology, v. 48, p.&amp;amp;nbsp;189-213.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Raiswell, R., and Q.J. Fisher, 2000, &#039;&#039;Mudrock-hosted carbonate concretions: a review of growth mechanisms and their influence on chemical and isotopic composition&#039;&#039;: Journal of Geological Society of London. v. 157, p.&amp;amp;nbsp;239-251&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Scotchman, I.C., 1991, &#039;&#039;The geochemistry of concretions from the Kimmeridge Clay Formation of southern and eastern England&#039;&#039;: Sedimentology. v. 38, pp.&amp;amp;nbsp;79–106.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Thyne, G.D., and J.R. Boles, 1989, &#039;&#039;Isotopic evidence for origin of the Moeraki septarian concretions, New Zealand&#039;&#039;: Journal of Sedimentary Petrology. v. 59, n. 2, pp.&amp;amp;nbsp;272–279.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Voigt, E., 1968, &#039;&#039;Uber-Hiatus-Konkretion (dargestellt an Beispielen aus dem Lias)&#039;&#039;: Geologische Rundschau. v. 58, pp.&amp;amp;nbsp;281–296.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Wilson, M.A., 1985, &#039;&#039;Disturbance and ecologic succession in an Upper Ordovician cobble-dwelling hardground fauna&#039;&#039;: Science. v. 228, pp.&amp;amp;nbsp;575–577.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Wilson, M.A., and Taylor, P.D., 2001, &#039;&#039;Palaeoecology of hard substrate faunas from the Cretaceous Qahlah Formation of the Oman Mountains&#039;&#039;: Palaeontology. v. 44, pp.&amp;amp;nbsp;21–41.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* Zaton, M., 2010, &#039;&#039;Hiatus concretions&#039;&#039;: Geology Today. v. 26, pp.&amp;amp;nbsp;186–189.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Pranala luar ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Pranala luar ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Dietrich, R.V., 2002, [https://web.archive.org/web/20081202111650/http://www.cst.cmich.edu/users/dietr1rv/concretions/index.htm &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;], The Wayback Machine. and [http://condor.cmich.edu/cdm/singleitem/collection/p1610-01coll1/id/3165/rec/4228 PDF file of &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;] , CMU Online Digital Object Repository, Central Michigan University, Mount Pleasant, Michigan.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Dietrich, R.V., 2002, [https://web.archive.org/web/20081202111650/http://www.cst.cmich.edu/users/dietr1rv/concretions/index.htm &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;], The Wayback Machine. and [http://condor.cmich.edu/cdm/singleitem/collection/p1610-01coll1/id/3165/rec/4228 PDF file of &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;] , CMU Online Digital Object Repository, Central Michigan University, Mount Pleasant, Michigan.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l47&quot;&gt;Baris 47:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Baris 18:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Heinrich, P.V., 2007, [http://www.hgms.org/BBG/Aug07.pdf &amp;#039;&amp;#039;The Giant Concretions of Rock City Kansas&amp;#039;&amp;#039; PDF version, 836 KB]  BackBender&amp;#039;s Gazette. vol. 38, no. 8, pp.&amp;amp;nbsp;6–12.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Heinrich, P.V., 2007, [http://www.hgms.org/BBG/Aug07.pdf &amp;#039;&amp;#039;The Giant Concretions of Rock City Kansas&amp;#039;&amp;#039; PDF version, 836 KB]  BackBender&amp;#039;s Gazette. vol. 38, no. 8, pp.&amp;amp;nbsp;6–12.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Hokianga Tourism Association, nd, [http://hokiangatourism.org.nz/activities/attractions/koutu-boulders &amp;#039;&amp;#039;Koutu Boulders ANY ONE FOR A GAME OF BOWLS?&amp;#039;&amp;#039;] and [http://www.hokianga.net.nz/hokianga/koutu/koutu_boulders.htm &amp;#039;&amp;#039;Koutu Boulders, Hokianga Harbour, Northland, New Zealand&amp;#039;&amp;#039;]  High-quality pictures of cannonball concretions.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Hokianga Tourism Association, nd, [http://hokiangatourism.org.nz/activities/attractions/koutu-boulders &amp;#039;&amp;#039;Koutu Boulders ANY ONE FOR A GAME OF BOWLS?&amp;#039;&amp;#039;] and [http://www.hokianga.net.nz/hokianga/koutu/koutu_boulders.htm &amp;#039;&amp;#039;Koutu Boulders, Hokianga Harbour, Northland, New Zealand&amp;#039;&amp;#039;]  High-quality pictures of cannonball concretions.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2006, [http://irna.lautre.net/Tout-ce-que-la-nature-ne-peut-pas,45.html All that nature can never do, part IV: stone spheres]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2006, [http://irna.lautre.net/Tout-ce-que-la-nature-ne-peut-pas,45.html All that nature can never do, part IV: stone spheres]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2007a, [http://irna.lautre.net/Stone-balls-in-France-too.html Stone balls: in France too!]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2007a, [http://irna.lautre.net/Stone-balls-in-France-too.html Stone balls: in France too!]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2007b, [http://irna.lautre.net/Boules-de-pierre-en-Slovaquie.html Stone balls in Slowakia, Czech Republic and Poland]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Irna, 2007b, [http://irna.lautre.net/Boules-de-pierre-en-Slovaquie.html Stone balls in Slowakia, Czech Republic and Poland]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Katz, B., 1998, [http://www.desertusa.com/mag98/oct/papr/geo_conc.html &amp;#039;&amp;#039;Concretions&amp;#039;&amp;#039;] Digital West Media, Inc.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Katz, B., 1998, [http://www.desertusa.com/mag98/oct/papr/geo_conc.html &amp;#039;&amp;#039;Concretions&amp;#039;&amp;#039;] Digital West Media, Inc.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Kuban, Glen J., 2006-2008. [http://paleo.cc/paluxy/nevada.htm Nevada Shoe Prints?]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Kuban, Glen J., 2006-2008. [http://paleo.cc/paluxy/nevada.htm Nevada Shoe Prints?]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* McCollum, A., nd, [http://allanmccollum.net/amcimages/imperialvalleyconcretions.html &amp;#039;&amp;#039;Sand Concretions from Imperial Valley&amp;#039;&amp;#039;], a collection of articles maintained by an American artist.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* McCollum, A., nd, [http://allanmccollum.net/amcimages/imperialvalleyconcretions.html &amp;#039;&amp;#039;Sand Concretions from Imperial Valley&amp;#039;&amp;#039;], a collection of articles maintained by an American artist.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Mozley, P.S., [http://allanmccollum.net/amcimages/mozley.html &amp;#039;&amp;#039;Concretions, bombs, and groundwater&amp;#039;&amp;#039;], on-line version of an overview paper originally published by the New Mexico Bureau of Geology and Mineral Resources.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Mozley, P.S., [http://allanmccollum.net/amcimages/mozley.html &amp;#039;&amp;#039;Concretions, bombs, and groundwater&amp;#039;&amp;#039;], on-line version of an overview paper originally published by the New Mexico Bureau of Geology and Mineral Resources.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* United States Geological Survey, nd, [http://nd.water.usgs.gov/lewisandclark/points/concretions.html &#039;&#039;Cannonball concretion&#039;&#039;]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* United States Geological Survey, nd, [http://nd.water.usgs.gov/lewisandclark/points/concretions.html &#039;&#039;Cannonball concretion&#039;&#039;]  &lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* University of Utah, 2004, [http://unews.utah.edu/news_releases/earth-has-039blueberries039-like-mars/ &amp;#039;&amp;#039;Earth Has &amp;#039;Blueberries&amp;#039; Like Mars &amp;#039;Moqui Marbles&amp;#039; Formed in Groundwater in Utah&amp;#039;s National Parks&amp;#039;&amp;#039;]  press release about iron oxide and Martian concretions&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* University of Utah, 2004, [http://unews.utah.edu/news_releases/earth-has-039blueberries039-like-mars/ &amp;#039;&amp;#039;Earth Has &amp;#039;Blueberries&amp;#039; Like Mars &amp;#039;Moqui Marbles&amp;#039; Formed in Groundwater in Utah&amp;#039;s National Parks&amp;#039;&amp;#039;]  press release about iron oxide and Martian concretions&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;== Sumber dan atribusi ==&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Konkresi+%28geologi%29&amp;amp;oldid=28451448 Wikipedia bahasa Indonesia], revisi 28451448 (2025-11-13T07:27:56Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Gambar pada artikel ini bersumber dari Wikimedia Commons dan mengikuti ketentuan lisensi masing-masing berkas. Mohon gunakan konten dan media secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;== Sumber dan atribusi ==&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;!&lt;/ins&gt;-- &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;WIKI_UNISSULA_PRESENTATION_V4 &lt;/ins&gt;--&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Konkresi+%28geologi%29&amp;amp;oldid=28451448 Wikipedia bahasa Indonesia], revisi 28451448 (2025&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;11&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;13T07:27:56Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;BerbagiSerupa (CC BY&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Maintenance script</name></author>
	</entry>
	<entry>
		<id>https://wiki.unissula.ac.id/index.php?title=Konkresi_(geologi)&amp;diff=20577&amp;oldid=prev</id>
		<title>Maintenance script: Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 28451448; atribusi sumber disertakan.</title>
		<link rel="alternate" type="text/html" href="https://wiki.unissula.ac.id/index.php?title=Konkresi_(geologi)&amp;diff=20577&amp;oldid=prev"/>
		<updated>2026-08-28T03:21:21Z</updated>

		<summary type="html">&lt;p&gt;Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 28451448; atribusi sumber disertakan.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Halaman baru&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Konkresi&amp;#039;&amp;#039;&amp;#039; adalah massa kompak yang keras, terbentuk dari presipitasi semen [[mineral]] di dalam rongga-rongga partikel, dan ditemukan di [[batuan sedimen]] atau [[tanah]]. Konkresi berbentuk seperti [[telur]] ataupun bulat, tetapi bentuk-bentuk iregular juga sering terjadi. Istilah &amp;#039;konkresi&amp;#039; berasal dari [[bahasa latin]] &amp;#039;&amp;#039;Con &amp;#039;&amp;#039;yang artinya &amp;#039;bersama&amp;#039; dan &amp;#039;&amp;#039;crescere &amp;#039;&amp;#039;yang artinya &amp;#039;tumbuh&amp;#039;. Konkresi-konkresi terbentuk di perlapisan strata sedimen yang telah terendapkan terlebih dahulu. Mereka biasanya terbentuk lebih awal ketika terjadi penumpukkan sedimen, sebelum kemudian sedimen tersebut mengeras menjadi [[batu]]an. Semen konkresi ini sering menyebabkan konkresi lebih keras dan lebih tahan terhadap pelapukan dibanding perlapisan induknya.&lt;br /&gt;
&lt;br /&gt;
Ada perbedaan penting antara konkresi dan [[nodula]]. Konkresi terbentuk dari presipitasi mineral di sekitar sejenis nukleus sedangkan nodula adalah tubuh yang tergantikan.&lt;br /&gt;
&lt;br /&gt;
Deskripsi yang telah dilakukan semenjak abad ke-18 membuktikan bahwa konkresi telah menarik perhatian ilmuan sejak masa lalu. Hal itu disebabkan adanya variasi bentuk yang tidak biasa, ukuran dan komposisi, yang membuatnya sempat dikira [[telur dinosaurus]], hewan, dan fosil tumbuhan, hingga puing antariksa atau [[artefak]] manusia.&lt;br /&gt;
&lt;br /&gt;
== Galeri ==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
== Sitasi ==&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
== Referensi ==&lt;br /&gt;
* Al-Agha, M.R., S.D. Burley, C.D. Curtis, and J. Esson, 1995, &amp;#039;&amp;#039;Complex cementation textures and authigenic mineral assemblages in Recent concretions from the Lincolnshire Wash (east coast, UK) driven by Fe(0) Fe(II) oxidation&amp;#039;&amp;#039;: Journal of the Geological Society, London, v. 152, pp.&amp;amp;nbsp;157–171.&lt;br /&gt;
* Boles, J.R., C.A. Landis, and P. Dale, 1985, [http://jsedres.sepmonline.org/cgi/content/abstract/55/3/398 &amp;#039;&amp;#039;The Moeraki Boulders; anatomy of some septarian concretions&amp;#039;&amp;#039;]:, Journal of Sedimentary Petrology. v. 55, n. 3, pp.&amp;amp;nbsp;398–406.&lt;br /&gt;
* Chan, M.A. and W.T. Parry, 2002, [http://geology.utah.gov/online/pdf/pi-77.pdf &amp;#039;&amp;#039;&amp;#039;Mysteries of Sandstone Colors and Concretions in Colorado Plateau Canyon Country&amp;#039;&amp;#039; PDF version, 468 KB] : Utah Geological Survey Public Information Series. n. 77, pp.&amp;amp;nbsp;1–19.&lt;br /&gt;
* Chan, M.A., B.B. Beitler, W.T. Parry, J. Ormo, and G. Komatsu, 2005. [ftp://rock.geosociety.org/pub/GSAToday/gt0508.pdf &amp;#039;&amp;#039;Red Rock and Red Planet Diagenesis: Comparison of Earth and Mars Concretions&amp;#039;&amp;#039; PDF version, 3.4 MB] : GSA Today, v. 15, n. 8, pp.&amp;amp;nbsp;4–10.&lt;br /&gt;
* Davis, J.M., 1999, &amp;#039;&amp;#039;Oriented carbonate concretions in a paleoaquifer: Insights into geologic controls on fluid flow&amp;#039;&amp;#039;: Water Resources Research, v. 35, p.&amp;amp;nbsp;1705-1712.&lt;br /&gt;
* Hattin, D.E., 1982, &amp;#039;&amp;#039;Stratigraphy and depositional environment of the Smoky Hill Chalk Member, Niobrara Chalk (Upper Cretaceous) of the type area, western Kansas&amp;#039;&amp;#039;: Kansas Geological Survey Bulletin 225:1-108.&lt;br /&gt;
* Hobbs, D., and J. Hafnaer, 1999, &amp;#039;&amp;#039;Magnetism and magneto-structural effects in transition-metal sulphides&amp;#039;&amp;#039;: Journal of Physics: Condensed Matter, v. 11, pp.&amp;amp;nbsp;8197–8222.&lt;br /&gt;
* Hoffmann, V., H. Stanjek, and E. Murad, 1993, &amp;#039;&amp;#039;Mineralogical, magnetic and mössbauer data of symthite (Fe9S11) &amp;#039;&amp;#039;: Studia Geophysica et Geodaetica, v. 37, pp.&amp;amp;nbsp;366–381.&lt;br /&gt;
* Johnson, M.R., 1989, &amp;#039;&amp;#039;Paleogeographic significance of oriented calcareous concretions in the Triassic Katberg Formation, South Africa&amp;#039;&amp;#039;: Journal of Sedimentary Petrology, v. 59, p.&amp;amp;nbsp;1008-1010.&lt;br /&gt;
* Loope D.B., Kettler R.M., Weber K.A., 2011, &amp;#039;&amp;#039;Morphologic Clues to the origin of Iron Oxide-Cemented Sphereoids, Boxworks, and Pipelike Concretions, Navajo Sandstone of South-Central Utah, U.S.A,&amp;#039;&amp;#039; The Journal of Geology, Vol. 119, No. 5 (September 2011), pp.&amp;amp;nbsp;505–520&lt;br /&gt;
* Loope D.B., Kettler R.M., Weber K.A., 2011, &amp;#039;&amp;#039;Follow the water: Connecting a CO2 reservoir and bleached sandstone to iron-rich concretions in the Navajo Sandstone of south-central Utah, USA,&amp;#039;&amp;#039; GEOLOGY FORUM, November 2011, Geological Society of America doi:10.1130/G32550Y.1&lt;br /&gt;
* McBride, E.F., M.D. Picard, and R.L. Folk, 1994, &amp;#039;&amp;#039;Oriented concretions, Ionian Coast, Italy: evidence of groundwater flow direction&amp;#039;&amp;#039;: Journal of Sedimentary Research, v. 64, p.&amp;amp;nbsp;535-540.&lt;br /&gt;
* McBride, E.F., M.D. Picard, and K.L. Milliken, 2003, [http://jsedres.sepmonline.org/cgi/content/abstract/73/3/462 &amp;#039;&amp;#039;Calcite-Cemented Concretions in Cretaceous Sandstone, Wyoming and Utah, U.S.A.&amp;#039;&amp;#039;]: Journal of Sedimentary Research. v. 73, n. 3, p.&amp;amp;nbsp;462-483.&lt;br /&gt;
* Mozley, P.S., 1996, &amp;#039;&amp;#039;The internal structure of carbonate concretions: A critical evaluation of the concentric model of concretion growth: Sedimentary Geology&amp;#039;&amp;#039;: v. 103, p.&amp;amp;nbsp;85-91.&lt;br /&gt;
* Mozley, P.S., and Goodwin, L., 1995, &amp;#039;&amp;#039;Patterns of cementation along a Cenozoic normal fault: A record of paleoflow orientations: Geology&amp;#039;&amp;#039;: v. 23, p 539-542.&lt;br /&gt;
* Mozley, P.S., and Burns, S.J., 1993, &amp;#039;&amp;#039;Oxygen and carbon isotopic composition of marine carbonate concretions: an overview: Journal of Sedimentary Petrology, v. 63, p. 73-83.&amp;#039;&amp;#039;&lt;br /&gt;
* Mozley, P.S., and Davis, J.M., 2005, &amp;#039;&amp;#039;Internal structure and mode of growth of elongate calcite concretions: Evidence for small-scale microbially induced, chemical heterogeneity in groundwater&amp;#039;&amp;#039;: Geological Society of America Bulletin, v. 117, 1400-1412.&lt;br /&gt;
* Pratt, B.R., 2001, &amp;quot;Septarian concretions: internal cracking caused by synsedimentary earthquakes&amp;quot;: Sedimentology, v. 48, p.&amp;amp;nbsp;189-213.&lt;br /&gt;
* Raiswell, R., and Q.J. Fisher, 2000, &amp;#039;&amp;#039;Mudrock-hosted carbonate concretions: a review of growth mechanisms and their influence on chemical and isotopic composition&amp;#039;&amp;#039;: Journal of Geological Society of London. v. 157, p.&amp;amp;nbsp;239-251&lt;br /&gt;
* Scotchman, I.C., 1991, &amp;#039;&amp;#039;The geochemistry of concretions from the Kimmeridge Clay Formation of southern and eastern England&amp;#039;&amp;#039;: Sedimentology. v. 38, pp.&amp;amp;nbsp;79–106.&lt;br /&gt;
* Thyne, G.D., and J.R. Boles, 1989, &amp;#039;&amp;#039;Isotopic evidence for origin of the Moeraki septarian concretions, New Zealand&amp;#039;&amp;#039;: Journal of Sedimentary Petrology. v. 59, n. 2, pp.&amp;amp;nbsp;272–279.&lt;br /&gt;
* Voigt, E., 1968, &amp;#039;&amp;#039;Uber-Hiatus-Konkretion (dargestellt an Beispielen aus dem Lias)&amp;#039;&amp;#039;: Geologische Rundschau. v. 58, pp.&amp;amp;nbsp;281–296.&lt;br /&gt;
* Wilson, M.A., 1985, &amp;#039;&amp;#039;Disturbance and ecologic succession in an Upper Ordovician cobble-dwelling hardground fauna&amp;#039;&amp;#039;: Science. v. 228, pp.&amp;amp;nbsp;575–577.&lt;br /&gt;
* Wilson, M.A., and Taylor, P.D., 2001, &amp;#039;&amp;#039;Palaeoecology of hard substrate faunas from the Cretaceous Qahlah Formation of the Oman Mountains&amp;#039;&amp;#039;: Palaeontology. v. 44, pp.&amp;amp;nbsp;21–41.&lt;br /&gt;
* Zaton, M., 2010, &amp;#039;&amp;#039;Hiatus concretions&amp;#039;&amp;#039;: Geology Today. v. 26, pp.&amp;amp;nbsp;186–189.&lt;br /&gt;
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== Pranala luar ==&lt;br /&gt;
* Dietrich, R.V., 2002, [https://web.archive.org/web/20081202111650/http://www.cst.cmich.edu/users/dietr1rv/concretions/index.htm &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;], The Wayback Machine. and [http://condor.cmich.edu/cdm/singleitem/collection/p1610-01coll1/id/3165/rec/4228 PDF file of &amp;#039;&amp;#039;Carbonate Concretions--A Bibliography&amp;#039;&amp;#039;] , CMU Online Digital Object Repository, Central Michigan University, Mount Pleasant, Michigan.&lt;br /&gt;
* Biek, B., 2002, [https://www.dmr.nd.gov/ndgs/ndnotes/concretions/concretions.asp &amp;#039;&amp;#039;Concretions and Nodules in North Dakota&amp;#039;&amp;#039;] North Dakota Geological Survey, Bismarck, North Dakota.&lt;br /&gt;
* Epoch Times Staff, 2007, [http://en.epochtimes.com/news/7-4-17/54224.html &amp;#039;&amp;#039;Mysterious Huge Stone Eggs Discovered in Hunan Province&amp;#039;&amp;#039;] Epoch Times International. Photographs of large cannonball concretions recently found in Hunan Province, China.&lt;br /&gt;
* Everhart, M., 2004, [http://www.oceansofkansas.com/FieldGuide5.html &amp;#039;&amp;#039;A Field Guide to Fossils of the Smoky Hill ChalkPart 5: Coprolites, Pearls, Fossilized Wood and other Remains&amp;#039;&amp;#039;] Part of the [http://www.oceansofkansas.com Oceans of Kansas] web site.&lt;br /&gt;
* Hansen, M.C., 1994, [http://www.ohiodnr.com/Portals/10/pdf/GeoFacts/geof04.pdf &amp;#039;&amp;#039;Ohio Shale Concretions&amp;#039;&amp;#039; PDF version, 270 KB]  Ohio Division of Geological Survey GeoFacts n. 4, pp.&amp;amp;nbsp;1–2.&lt;br /&gt;
* Hanson, W.D., and J.M. Howard, 2005, [http://geology.ar.gov/mis_pub_info/MP%2022%20Prim%20Boulders.pdf &amp;#039;&amp;#039;Spherical Boulders in North-Central Arkansas&amp;#039;&amp;#039; PDF version, 2.8 MB]  Arkansas Geological Commission Miscellaneous Publication n. 22, pp.&amp;amp;nbsp;1–23.&lt;br /&gt;
* Heinrich, P.V., 2007, [http://www.hgms.org/BBG/Aug07.pdf &amp;#039;&amp;#039;The Giant Concretions of Rock City Kansas&amp;#039;&amp;#039; PDF version, 836 KB]  BackBender&amp;#039;s Gazette. vol. 38, no. 8, pp.&amp;amp;nbsp;6–12.&lt;br /&gt;
* Hokianga Tourism Association, nd, [http://hokiangatourism.org.nz/activities/attractions/koutu-boulders &amp;#039;&amp;#039;Koutu Boulders ANY ONE FOR A GAME OF BOWLS?&amp;#039;&amp;#039;] and [http://www.hokianga.net.nz/hokianga/koutu/koutu_boulders.htm &amp;#039;&amp;#039;Koutu Boulders, Hokianga Harbour, Northland, New Zealand&amp;#039;&amp;#039;]  High-quality pictures of cannonball concretions.&lt;br /&gt;
* Irna, 2006, [http://irna.lautre.net/Tout-ce-que-la-nature-ne-peut-pas,45.html All that nature can never do, part IV: stone spheres]&lt;br /&gt;
* Irna, 2007a, [http://irna.lautre.net/Stone-balls-in-France-too.html Stone balls: in France too!]&lt;br /&gt;
* Irna, 2007b, [http://irna.lautre.net/Boules-de-pierre-en-Slovaquie.html Stone balls in Slowakia, Czech Republic and Poland]&lt;br /&gt;
* Katz, B., 1998, [http://www.desertusa.com/mag98/oct/papr/geo_conc.html &amp;#039;&amp;#039;Concretions&amp;#039;&amp;#039;] Digital West Media, Inc.&lt;br /&gt;
* Kuban, Glen J., 2006-2008. [http://paleo.cc/paluxy/nevada.htm Nevada Shoe Prints?]&lt;br /&gt;
* McCollum, A., nd, [http://allanmccollum.net/amcimages/imperialvalleyconcretions.html &amp;#039;&amp;#039;Sand Concretions from Imperial Valley&amp;#039;&amp;#039;], a collection of articles maintained by an American artist.&lt;br /&gt;
* Mozley, P.S., [http://allanmccollum.net/amcimages/mozley.html &amp;#039;&amp;#039;Concretions, bombs, and groundwater&amp;#039;&amp;#039;], on-line version of an overview paper originally published by the New Mexico Bureau of Geology and Mineral Resources.&lt;br /&gt;
* United States Geological Survey, nd, [http://nd.water.usgs.gov/lewisandclark/points/concretions.html &amp;#039;&amp;#039;Cannonball concretion&amp;#039;&amp;#039;]&lt;br /&gt;
* University of Utah, 2004, [http://unews.utah.edu/news_releases/earth-has-039blueberries039-like-mars/ &amp;#039;&amp;#039;Earth Has &amp;#039;Blueberries&amp;#039; Like Mars &amp;#039;Moqui Marbles&amp;#039; Formed in Groundwater in Utah&amp;#039;s National Parks&amp;#039;&amp;#039;]  press release about iron oxide and Martian concretions&lt;br /&gt;
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== Sumber dan atribusi ==&lt;br /&gt;
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Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Konkresi+%28geologi%29&amp;amp;oldid=28451448 Wikipedia bahasa Indonesia], revisi 28451448 (2025-11-13T07:27:56Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.&lt;/div&gt;</summary>
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