https://wiki.unissula.ac.id/index.php?action=history&feed=atom&title=Endapan_bijih_sulfida_masif_vulkanogenikEndapan bijih sulfida masif vulkanogenik - Riwayat revisi2026-09-16T04:18:17ZRiwayat revisi halaman ini di wikiMediaWiki 1.46.0https://wiki.unissula.ac.id/index.php?title=Endapan_bijih_sulfida_masif_vulkanogenik&diff=15409&oldid=prevMaintenance script: Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi2026-08-26T18:04:22Z<p>Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi</p>
<table style="background-color: #fff; color: #202122;" data-mw-interface="">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="id">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Revisi sebelumnya</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revisi per 26 Agustus 2026 18.04</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l16">Baris 16:</td>
<td colspan="2" class="diff-lineno">Baris 16:</td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>* [[Vulkanologi]]</div></td><td class="diff-marker"></td><td style="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;"><div>* [[Vulkanologi]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>* [[Hidrotermal]]</div></td><td class="diff-marker"></td><td style="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;"><div>* [[Hidrotermal]]</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">== Referensi ==</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Barrie, C. T., and Hannington, M. D., editors, (1999), ''Volcanic-Associated Massive Sulfide Deposits: Processes and Examples in Modern and Ancient Settings'', Reviews in Economic Geology Volume 8, Society of Economic Geologists, Denver, 408 p.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Barrie, C. T., and Hannington, M. D., 1999, Classification of volcanic-associated massive sulfide deposits based on host-rock composition: Reviews in Economic Geology, v. 8, p. 1-11.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Franklin, J. M., Sangster, D. M., and Lydon, J. W., 1981, Volcanic-associated massive sulfide deposits, in Skinner, B. J., ed., Economic Geology Seventy-Fifth Anniversary Volume, Society of Economic Geologists, p. 485-627.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Franklin, J. M., Gibson, H. L., Galley, A. G., and Jonasson, I. R., 2005, Volcanogenic Massive Sulfide Deposits, in Hedenquist, J. W., Thompson, J. F. H., Goldfarb, R. J., and Richards, J. P., eds., Economic Geology 100th Anniversary Volume: Littleton, CO, Society of Economic Geologists, p. 523-560.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Guilbert, John M., and Charles F. Park, Jr., 1986, ''The Geology of Ore Deposits'', pp 572-603, W. H. Freeman, [[Special:BookSources/0716714566|ISBN 0-7167-1456-6]]</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Gibson, Harold L., James M. Franklin, and Mark D. Hannington, (2000) ''A genetic model for Volcanic-Associated Massive Sulphide Deposits'' http://www.cseg.ca/conferences/2000/2000abstracts/758.PDF Accessed 12-20-2005.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;">* Lydon, J. W., 1984, Ore deposit models; 8, Volcanogenic sulfide deposits; Part I, A descriptive model: Geoscience Canada, v. 11, p. 195-202.</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><br></td><td class="diff-marker"></td><td style="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;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>== Pranala luar ==</div></td><td class="diff-marker"></td><td style="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;"><div>== Pranala luar ==</div></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>* [http://www.eurekalert.org/pub_releases/2006-02/nsae-tdo021706.php ''The dawn of deep ocean mining,'' Steven Scott, Feb. 2006]</div></td><td class="diff-marker"></td><td style="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;"><div>* [http://www.eurekalert.org/pub_releases/2006-02/nsae-tdo021706.php ''The dawn of deep ocean mining,'' Steven Scott, Feb. 2006]</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="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;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><br></td><td class="diff-marker"></td><td style="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;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>== Sumber dan atribusi ==</div></td><td class="diff-marker"></td><td style="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;"><div>== Sumber dan atribusi ==</div></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><br></td><td class="diff-marker"></td><td style="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;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="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;"><div>Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Endapan+bijih+sulfida+masif+vulkanogenik&oldid=26525675 Wikipedia bahasa Indonesia], revisi 26525675 (2024-11-14T22:03:52Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</div></td><td class="diff-marker"></td><td style="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;"><div>Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Endapan+bijih+sulfida+masif+vulkanogenik&oldid=26525675 Wikipedia bahasa Indonesia], revisi 26525675 (2024-11-14T22:03:52Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="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;"><div><ins style="font-weight: bold; text-decoration: none;"></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="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;"><div><ins style="font-weight: bold; text-decoration: none;"><!-- WIKI_UNISSULA_PRESENTATION_V4 --></ins></div></td></tr>
</table>Maintenance scripthttps://wiki.unissula.ac.id/index.php?title=Endapan_bijih_sulfida_masif_vulkanogenik&diff=15010&oldid=prevMaintenance script: Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 26525675; atribusi sumber disertakan.2026-08-26T17:24:16Z<p>Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 26525675; atribusi sumber disertakan.</p>
<p><b>Halaman baru</b></p><div>'''Endapan bijih sulfida masif (''Volcanogenic massive sulfide'' / VMS) '''adalah sebuah tipe endapan bijih sulfida metal, yang terdiri dari terutama [[tembaga]] dan [[seng]] yang berasosiasi dan berasal dari kejadian [[hidrotermal]] vulkanik di lingkungan submarin.<br />
<br />
Endapan ini sering juga disebut endapan ''volcanic-hosted massive sulfide ''(VHMS). Massa jenisnya pada umumnya adalah 4500 Kg/m<sup>3</sup>. Endapan VMS kebanyakan merupakan akumulasi [[stratiform]] dari mineral-mineral [[sulfida]] yang [[Presipitasi (meteorologi)|terpresipitasi]] dari cairan hidrotermal diatas atau dibawah [[lantai samudra]] pada [[skala waktu geologi]] dari yang kuno hingga yang modern. Di samudra modern mereka sangat mirip dengan lidah-lidah sulfur yang biasa disebut [[asap hitam]] (''black smoker).''<br />
<br />
Mereka terbentuk di lingkungan yang didominasi oleh proses [[vulkanisme]] atau di lingkungan asal vulkanik (contoh, sedimen vulkanik), dan pengendapan terjadi bersamaan dengan pembentukan batuan vulkanik tersebut. Tipe endapan ini merepresentasikan sumber yang signifikan dari tembaga, seng, [[timbal]], [[emas]], dan bijih [[perak]], dengan [[kobalt]], [[timah]], [[barium]], [[sulfur]], [[selenium]], [[mangan]], [[kadmium]], [[indium]], [[bismuth]], [[telurium]], [[galium]], dan [[germanium]] juga hadir sebagai produk sampingan maupun produk yang berasal dari proses berbeda di tempat yang sama.<br />
<br />
Endapat sulfida masif vulkanogenik yang terbentuk saat ini berada di lantai samudra di sekitar [[gunungapi bawah laut]] bersama dengan [[punggung tengah samudra]], selain juga berada di [[cekungan busur belakang]] dan busur depan apungan (''rift). ''Banyak perusahaan eksplorasi [[mineral]] saat ini sedang mengeksplorasi endapan sulfida masif lantai samudra; Meskipun begitu sebagian besar eksplorasi terkonsentrasi dalam mencari ekuivalen endapan yang ada di darat.<br />
<br />
Kedekatannya dengan pusat erupsi dan [[batuan vulkanik]] membuat endapan VMS agak berbeda dengan tipe endapan sejenis yang memiliki sumber, cara transportasi, dan pemerangkapan yang sama. Endapan VMS dibedakan dengan endapan bijih lain karena terbentuk dekat dengan wilayah vulkanisme submarin dan terbentuk oleh sirkulasi hidrotermal dan ekshalasi sulfida yang tidak bergantung dengan proses-proses [[sedimentasi]], dimana endapan yang bergantung dengan proses-proses sedimentasi ini disebut endapan SEDEX (''sedimentary exhalative ''atau sedimentasi ekshalasif).<br />
<br />
Ada sebuah subkelas dari endapan VMS, yang memiliki karakteristik yang berada di antara endapan SEDEX dan VMS. Contohnya adalah endapan ''Bathurst camp, ''[[New brunswick]], [[Kanada]].<br />
<br />
== Lihat juga ==<br />
* [[Genesa bijih]]<br />
* [[Bijih]]<br />
* [[Vulkanologi]]<br />
* [[Hidrotermal]]<br />
<br />
== Referensi ==<br />
* Barrie, C. T., and Hannington, M. D., editors, (1999), ''Volcanic-Associated Massive Sulfide Deposits: Processes and Examples in Modern and Ancient Settings'', Reviews in Economic Geology Volume 8, Society of Economic Geologists, Denver, 408 p.<br />
* Barrie, C. T., and Hannington, M. D., 1999, Classification of volcanic-associated massive sulfide deposits based on host-rock composition: Reviews in Economic Geology, v. 8, p. 1-11.<br />
* Franklin, J. M., Sangster, D. M., and Lydon, J. W., 1981, Volcanic-associated massive sulfide deposits, in Skinner, B. J., ed., Economic Geology Seventy-Fifth Anniversary Volume, Society of Economic Geologists, p. 485-627.<br />
* Franklin, J. M., Gibson, H. L., Galley, A. G., and Jonasson, I. R., 2005, Volcanogenic Massive Sulfide Deposits, in Hedenquist, J. W., Thompson, J. F. H., Goldfarb, R. J., and Richards, J. P., eds., Economic Geology 100th Anniversary Volume: Littleton, CO, Society of Economic Geologists, p. 523-560.<br />
* Guilbert, John M., and Charles F. Park, Jr., 1986, ''The Geology of Ore Deposits'', pp 572-603, W. H. Freeman, [[Special:BookSources/0716714566|ISBN 0-7167-1456-6]]<br />
* Gibson, Harold L., James M. Franklin, and Mark D. Hannington, (2000) ''A genetic model for Volcanic-Associated Massive Sulphide Deposits'' http://www.cseg.ca/conferences/2000/2000abstracts/758.PDF Accessed 12-20-2005.<br />
* Lydon, J. W., 1984, Ore deposit models; 8, Volcanogenic sulfide deposits; Part I, A descriptive model: Geoscience Canada, v. 11, p. 195-202.<br />
<br />
== Pranala luar ==<br />
* [http://www.eurekalert.org/pub_releases/2006-02/nsae-tdo021706.php ''The dawn of deep ocean mining,'' Steven Scott, Feb. 2006]<br />
<br />
<br />
<br />
== Sumber dan atribusi ==<br />
<br />
Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Endapan+bijih+sulfida+masif+vulkanogenik&oldid=26525675 Wikipedia bahasa Indonesia], revisi 26525675 (2024-11-14T22:03:52Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</div>Maintenance script