Standard

Indium in cassiterite and ores of tin deposits. / Pavlova, G. G.; Palessky, S. V.; Borisenko, A. S. и др.

в: Ore Geology Reviews, Том 66, 01.04.2015, стр. 99-113.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Pavlova, GG, Palessky, SV, Borisenko, AS, Vladimirov, AG, Seifert, T & Phan, LA 2015, 'Indium in cassiterite and ores of tin deposits', Ore Geology Reviews, Том. 66, стр. 99-113. https://doi.org/10.1016/j.oregeorev.2014.10.009

APA

Pavlova, G. G., Palessky, S. V., Borisenko, A. S., Vladimirov, A. G., Seifert, T., & Phan, L. A. (2015). Indium in cassiterite and ores of tin deposits. Ore Geology Reviews, 66, 99-113. https://doi.org/10.1016/j.oregeorev.2014.10.009

Vancouver

Pavlova GG, Palessky SV, Borisenko AS, Vladimirov AG, Seifert T, Phan LA. Indium in cassiterite and ores of tin deposits. Ore Geology Reviews. 2015 апр. 1;66:99-113. doi: 10.1016/j.oregeorev.2014.10.009

Author

Pavlova, G. G. ; Palessky, S. V. ; Borisenko, A. S. и др. / Indium in cassiterite and ores of tin deposits. в: Ore Geology Reviews. 2015 ; Том 66. стр. 99-113.

BibTeX

@article{ca2d19a2d5b64e50a77799ba8ae26a3e,
title = "Indium in cassiterite and ores of tin deposits",
abstract = "The results obtained with LA-ICP-MS by less abundant lighter 113In isotope and EPMA show that in cassiterite of cassiterite-quartz veins the indium contents do not exceed 160ppm, while cassiterite from Sn-sulfide veins is characterized by higher indium contents from 40 to 485ppm; sulfides of Sn-sulfide veins unlike sulfides of cassiterite-quartz veins also have the highest indium contents: Fe-sphalerite (100-25,000ppm), chalcopyrite (up to 1000ppm), and stannite (up to 60,000ppm). Indium contents in the Sn-sulfide ore of the Tigrinoe and Pravourmiiskoe deposits obtained using SR-XRF, ICP-MS and atomic absorption methods range from 10 to 433ppm with average values of 56-65ppm. Indium-rich Sn-sulfide mineralization in five large Sn-Ag ore districts of the Far East Russia (Khingansky, Badzhalsky, Komsomolsky, Arminsky, Kavalerovsky) provides the impetus for further exploration of deposits with Sn-sulfide mineralization as the most promising indium resources in Russia. Empirical observations from geology and geochronology of cassiterite-quartz and Sn-sulfide mineralization show that the combined contribution from granite and alkaline-subalkaline mafic sources and multistage ore-forming processes doubled indium resources of deposits being the main factors in the formation of high grade indium mineralization.",
keywords = "High grade indium ore, Indium, Indium content detection, Russia Far East, Sn-In polymetallic ore, Sn-sulfide mineralization",
author = "Pavlova, {G. G.} and Palessky, {S. V.} and Borisenko, {A. S.} and Vladimirov, {A. G.} and Th Seifert and Phan, {Luu Anh}",
year = "2015",
month = apr,
day = "1",
doi = "10.1016/j.oregeorev.2014.10.009",
language = "English",
volume = "66",
pages = "99--113",
journal = "Ore Geology Reviews",
issn = "0169-1368",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Indium in cassiterite and ores of tin deposits

AU - Pavlova, G. G.

AU - Palessky, S. V.

AU - Borisenko, A. S.

AU - Vladimirov, A. G.

AU - Seifert, Th

AU - Phan, Luu Anh

PY - 2015/4/1

Y1 - 2015/4/1

N2 - The results obtained with LA-ICP-MS by less abundant lighter 113In isotope and EPMA show that in cassiterite of cassiterite-quartz veins the indium contents do not exceed 160ppm, while cassiterite from Sn-sulfide veins is characterized by higher indium contents from 40 to 485ppm; sulfides of Sn-sulfide veins unlike sulfides of cassiterite-quartz veins also have the highest indium contents: Fe-sphalerite (100-25,000ppm), chalcopyrite (up to 1000ppm), and stannite (up to 60,000ppm). Indium contents in the Sn-sulfide ore of the Tigrinoe and Pravourmiiskoe deposits obtained using SR-XRF, ICP-MS and atomic absorption methods range from 10 to 433ppm with average values of 56-65ppm. Indium-rich Sn-sulfide mineralization in five large Sn-Ag ore districts of the Far East Russia (Khingansky, Badzhalsky, Komsomolsky, Arminsky, Kavalerovsky) provides the impetus for further exploration of deposits with Sn-sulfide mineralization as the most promising indium resources in Russia. Empirical observations from geology and geochronology of cassiterite-quartz and Sn-sulfide mineralization show that the combined contribution from granite and alkaline-subalkaline mafic sources and multistage ore-forming processes doubled indium resources of deposits being the main factors in the formation of high grade indium mineralization.

AB - The results obtained with LA-ICP-MS by less abundant lighter 113In isotope and EPMA show that in cassiterite of cassiterite-quartz veins the indium contents do not exceed 160ppm, while cassiterite from Sn-sulfide veins is characterized by higher indium contents from 40 to 485ppm; sulfides of Sn-sulfide veins unlike sulfides of cassiterite-quartz veins also have the highest indium contents: Fe-sphalerite (100-25,000ppm), chalcopyrite (up to 1000ppm), and stannite (up to 60,000ppm). Indium contents in the Sn-sulfide ore of the Tigrinoe and Pravourmiiskoe deposits obtained using SR-XRF, ICP-MS and atomic absorption methods range from 10 to 433ppm with average values of 56-65ppm. Indium-rich Sn-sulfide mineralization in five large Sn-Ag ore districts of the Far East Russia (Khingansky, Badzhalsky, Komsomolsky, Arminsky, Kavalerovsky) provides the impetus for further exploration of deposits with Sn-sulfide mineralization as the most promising indium resources in Russia. Empirical observations from geology and geochronology of cassiterite-quartz and Sn-sulfide mineralization show that the combined contribution from granite and alkaline-subalkaline mafic sources and multistage ore-forming processes doubled indium resources of deposits being the main factors in the formation of high grade indium mineralization.

KW - High grade indium ore

KW - Indium

KW - Indium content detection

KW - Russia Far East

KW - Sn-In polymetallic ore

KW - Sn-sulfide mineralization

UR - http://www.scopus.com/inward/record.url?scp=84920611784&partnerID=8YFLogxK

U2 - 10.1016/j.oregeorev.2014.10.009

DO - 10.1016/j.oregeorev.2014.10.009

M3 - Article

AN - SCOPUS:84920611784

VL - 66

SP - 99

EP - 113

JO - Ore Geology Reviews

JF - Ore Geology Reviews

SN - 0169-1368

ER -

ID: 25469998