Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka
The Asachinskoe epithermal gold deposit in South Kamchatka, Russia, is a low-sulfidation type deposit which consists of Au-Ag bearing quartz-adularia-illite veins. Cathodoluminescence (CL) analysis using optical microscope and scanning electron microscope and trace element analysis of quartz using e...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.564.6781 2023-05-15T16:58:56+02:00 Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka Ryohei Takahashi Axel Müller Hiroharu Matsueda Victor M. Okrugin Shuji Ono Alfons Van Den Kerkhof Andreas Kronz Elena D. Andreeva The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.6781 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.6781 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf Cathodoluminescence Trace Element Quartz Epithermal Gold deposit Asachinskoe text ftciteseerx 2016-01-08T12:12:26Z The Asachinskoe epithermal gold deposit in South Kamchatka, Russia, is a low-sulfidation type deposit which consists of Au-Ag bearing quartz-adularia-illite veins. Cathodoluminescence (CL) analysis using optical microscope and scanning electron microscope and trace element analysis of quartz using electron probe micro-analyzer (EPMA) were performed to elucidate the relationships between CL structures, trace element concentrations of different quartz generations, and metal pre-cipitation mechanism of the Asachinskoe deposit. Five sequences of quartz crystallization can be distinguished within the mineralized vein of the bonanza zone. Most distinctive trace elements in quartz are Al (av. 1463 ppm) and K (av. 350 ppm). Colloform and microcrystalline quartz with moderate to dull red-brown CL coexists with electrum (Au-Ag alloy), naumannite-aguilarite (ss) and polybasite-pearceite (ss). The Au-Ag-Se precipitation is related to fluid boiling, and the Se en-richment is attributed to relative oxidizing mineralization conditions. Almost non-luminescent, dark brown luminescent quartz forming the matrix of the hydrothermal breccia coexists with elec-trum, tetrahedrite-tennantite (ss) and covellite. The Au-Ag-Cu precipitation is associated with rap-idly precipitated quartz and adularia, and is due to sudden decompression and fluid boiling related to the hydrothermal brecciation. Text Kamchatka Unknown Bonanza ENVELOPE(-119.820,-119.820,55.917,55.917) |
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ftciteseerx |
language |
English |
topic |
Cathodoluminescence Trace Element Quartz Epithermal Gold deposit Asachinskoe |
spellingShingle |
Cathodoluminescence Trace Element Quartz Epithermal Gold deposit Asachinskoe Ryohei Takahashi Axel Müller Hiroharu Matsueda Victor M. Okrugin Shuji Ono Alfons Van Den Kerkhof Andreas Kronz Elena D. Andreeva Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
topic_facet |
Cathodoluminescence Trace Element Quartz Epithermal Gold deposit Asachinskoe |
description |
The Asachinskoe epithermal gold deposit in South Kamchatka, Russia, is a low-sulfidation type deposit which consists of Au-Ag bearing quartz-adularia-illite veins. Cathodoluminescence (CL) analysis using optical microscope and scanning electron microscope and trace element analysis of quartz using electron probe micro-analyzer (EPMA) were performed to elucidate the relationships between CL structures, trace element concentrations of different quartz generations, and metal pre-cipitation mechanism of the Asachinskoe deposit. Five sequences of quartz crystallization can be distinguished within the mineralized vein of the bonanza zone. Most distinctive trace elements in quartz are Al (av. 1463 ppm) and K (av. 350 ppm). Colloform and microcrystalline quartz with moderate to dull red-brown CL coexists with electrum (Au-Ag alloy), naumannite-aguilarite (ss) and polybasite-pearceite (ss). The Au-Ag-Se precipitation is related to fluid boiling, and the Se en-richment is attributed to relative oxidizing mineralization conditions. Almost non-luminescent, dark brown luminescent quartz forming the matrix of the hydrothermal breccia coexists with elec-trum, tetrahedrite-tennantite (ss) and covellite. The Au-Ag-Cu precipitation is associated with rap-idly precipitated quartz and adularia, and is due to sudden decompression and fluid boiling related to the hydrothermal brecciation. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Ryohei Takahashi Axel Müller Hiroharu Matsueda Victor M. Okrugin Shuji Ono Alfons Van Den Kerkhof Andreas Kronz Elena D. Andreeva |
author_facet |
Ryohei Takahashi Axel Müller Hiroharu Matsueda Victor M. Okrugin Shuji Ono Alfons Van Den Kerkhof Andreas Kronz Elena D. Andreeva |
author_sort |
Ryohei Takahashi |
title |
Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
title_short |
Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
title_full |
Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
title_fullStr |
Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
title_full_unstemmed |
Cathodoluminescence and Trace Elements in Quartz: Clues to Metal Precipitation Mechanisms at the Asachinskoe Gold Deposit in Kamchatka |
title_sort |
cathodoluminescence and trace elements in quartz: clues to metal precipitation mechanisms at the asachinskoe gold deposit in kamchatka |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.6781 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf |
long_lat |
ENVELOPE(-119.820,-119.820,55.917,55.917) |
geographic |
Bonanza |
geographic_facet |
Bonanza |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.6781 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/38463/1/p175-184-origin08.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766051070172200960 |