Minerals of the Au-Ag-Pb-Te-Se-S system of porphyry-copper-molybdenum deposits from the Nakhodka ore field, Chukchi Peninsula, Russia
The Nakhodka ore field located 220 km south of the Bilibino town, Chukchi Peninsula, Russia comprises Cu-Mo-porphyry (Malysh and Vesennii) and Mo-Cu-porphyry (Nakhodka, III Vesennii) deposits. The late epithermal mineralization with native gold of low fineness (498–766) of the first group deposits r...
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| Veröffentlicht in: | Moscow University geology bulletin 2012-07, Vol.67 (4), p.233-239 |
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| creator | Nagornaya, E. V. Baksheev, I. A. Bryzgalov, I. A. Yapaskurt, V. O. |
| description | The Nakhodka ore field located 220 km south of the Bilibino town, Chukchi Peninsula, Russia comprises Cu-Mo-porphyry (Malysh and Vesennii) and Mo-Cu-porphyry (Nakhodka, III Vesennii) deposits. The late epithermal mineralization with native gold of low fineness (498–766) of the first group deposits refers to the IS (intermediate sulfidation) type, which is characterized by the occurrence of petzite; stutzite; acanthite; pearceite; and minerals of the Pb-Bi-Ag-Se-Te, Ag-Te-Se, and Ag-Bi-Se systems, as well as by native tellurium. The epithermal mineralization forms at
f
Te
2
(−19...−18) and
f
S
2
(−14...−13) and temperatures |
| doi_str_mv | 10.3103/S0145875212040072 |
| format | Article |
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f
Te
2
(−19...−18) and
f
S
2
(−14...−13) and temperatures <200°C. The second group deposits do not exhibit epithermal mineralization; telluride mineralization is present as only native tellurium and altaite.</description><identifier>ISSN: 0145-8752</identifier><identifier>EISSN: 1934-8436</identifier><identifier>DOI: 10.3103/S0145875212040072</identifier><language>eng</language><publisher>Heidelberg: Allerton Press, Inc</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geology ; Gold ; Metals ; Mineralization ; Mineralogy ; Minerals ; Molybdenum ; Tellurium</subject><ispartof>Moscow University geology bulletin, 2012-07, Vol.67 (4), p.233-239</ispartof><rights>Allerton Press, Inc. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c349t-5d1d533c6399e606032a7d7bb4d78fafdd9a0079b92e56448a4fd66358d2d58e3</citedby><cites>FETCH-LOGICAL-c349t-5d1d533c6399e606032a7d7bb4d78fafdd9a0079b92e56448a4fd66358d2d58e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.3103/S0145875212040072$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.3103/S0145875212040072$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Nagornaya, E. V.</creatorcontrib><creatorcontrib>Baksheev, I. A.</creatorcontrib><creatorcontrib>Bryzgalov, I. A.</creatorcontrib><creatorcontrib>Yapaskurt, V. O.</creatorcontrib><title>Minerals of the Au-Ag-Pb-Te-Se-S system of porphyry-copper-molybdenum deposits from the Nakhodka ore field, Chukchi Peninsula, Russia</title><title>Moscow University geology bulletin</title><addtitle>Moscow Univ. Geol. Bull</addtitle><description>The Nakhodka ore field located 220 km south of the Bilibino town, Chukchi Peninsula, Russia comprises Cu-Mo-porphyry (Malysh and Vesennii) and Mo-Cu-porphyry (Nakhodka, III Vesennii) deposits. The late epithermal mineralization with native gold of low fineness (498–766) of the first group deposits refers to the IS (intermediate sulfidation) type, which is characterized by the occurrence of petzite; stutzite; acanthite; pearceite; and minerals of the Pb-Bi-Ag-Se-Te, Ag-Te-Se, and Ag-Bi-Se systems, as well as by native tellurium. The epithermal mineralization forms at
f
Te
2
(−19...−18) and
f
S
2
(−14...−13) and temperatures <200°C. The second group deposits do not exhibit epithermal mineralization; telluride mineralization is present as only native tellurium and altaite.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Gold</subject><subject>Metals</subject><subject>Mineralization</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Molybdenum</subject><subject>Tellurium</subject><issn>0145-8752</issn><issn>1934-8436</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kc1O3DAUhS1UJKYDD8DOUjdd4NaO7ThejkalrQRlxMA6cuIbEiaJUztZ5AF4bxymi6oV0pXu4nzn6P4gdMnoF84o_7qnTMhMyYQlVFCqkhO0YpoLkgmefkCrRSaLfoY-hvBMqZRa0BV6uW168KYN2FV4rAFvJrJ5IruCPADZx8JhDiN0izw4P9Szn0nphgE86Vw7Fxb6qcMWBheaMeDKu-4t55c51M4eDHYecNVAa6_wtp4OZd3gHfRNH6bWXOH7KYTGnKPTKs4AF3_6Gj1ef3vY_iA3d99_bjc3pORCj0RaZiXnZcq1hpSmlCdGWVUUwqqsMpW12sTddaETkKkQmRGVTVMuM5tYmQFfo8_H3MG73xOEMe-aUELbmh7cFHKmtBBaSaYi-ukf9NlNvo_T5fHeSilG42nXiB2p0rsQPFT54JvO-DlC-fKY_L_HRE9y9ITI9k_g_05-z_QKLpiO9Q</recordid><startdate>20120701</startdate><enddate>20120701</enddate><creator>Nagornaya, E. 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V.</au><au>Baksheev, I. A.</au><au>Bryzgalov, I. A.</au><au>Yapaskurt, V. O.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Minerals of the Au-Ag-Pb-Te-Se-S system of porphyry-copper-molybdenum deposits from the Nakhodka ore field, Chukchi Peninsula, Russia</atitle><jtitle>Moscow University geology bulletin</jtitle><stitle>Moscow Univ. Geol. Bull</stitle><date>2012-07-01</date><risdate>2012</risdate><volume>67</volume><issue>4</issue><spage>233</spage><epage>239</epage><pages>233-239</pages><issn>0145-8752</issn><eissn>1934-8436</eissn><abstract>The Nakhodka ore field located 220 km south of the Bilibino town, Chukchi Peninsula, Russia comprises Cu-Mo-porphyry (Malysh and Vesennii) and Mo-Cu-porphyry (Nakhodka, III Vesennii) deposits. The late epithermal mineralization with native gold of low fineness (498–766) of the first group deposits refers to the IS (intermediate sulfidation) type, which is characterized by the occurrence of petzite; stutzite; acanthite; pearceite; and minerals of the Pb-Bi-Ag-Se-Te, Ag-Te-Se, and Ag-Bi-Se systems, as well as by native tellurium. The epithermal mineralization forms at
f
Te
2
(−19...−18) and
f
S
2
(−14...−13) and temperatures <200°C. The second group deposits do not exhibit epithermal mineralization; telluride mineralization is present as only native tellurium and altaite.</abstract><cop>Heidelberg</cop><pub>Allerton Press, Inc</pub><doi>10.3103/S0145875212040072</doi><tpages>7</tpages></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences Geochemistry Geology Gold Metals Mineralization Mineralogy Minerals Molybdenum Tellurium |
| title | Minerals of the Au-Ag-Pb-Te-Se-S system of porphyry-copper-molybdenum deposits from the Nakhodka ore field, Chukchi Peninsula, Russia |
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