Indium in cassiterite and ores of tin deposits
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 160 ppm, while cassiterite from Sn-sulfide veins is characterized by higher indium contents from 40 to 485 ppm; sulfides of Sn-su...
Published in: | Ore geology reviews Vol. 66. P. 99-113 |
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Corporate Author: | |
Other Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Online Access: | http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000529051 Перейти в каталог НБ ТГУ |
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024 | 7 | |a 10.1016/j.oregeorev.2014.10.009 |2 doi | |
035 | |a to000529051 | ||
039 | 9 | |a 201812021547 |c 201604060757 |d cat202 |c 201604041622 |d VLOAD |y 201604041613 |z Александр Эльверович Гилязов | |
040 | |a RU-ToGU |b rus |c RU-ToGU | ||
245 | 1 | 0 | |a Indium in cassiterite and ores of tin deposits |c G. G. Pavlovaa, S. V. Palesskya, A. S. Borisenko [et.al.] |
504 | |a Библиогр.: с. 111-113. | ||
520 | 3 | |a 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 160 ppm, while cassiterite from Sn-sulfide veins is characterized by higher indium contents from 40 to 485 ppm; sulfides of Sn-sulfide veins unlike sulfides of cassiterite-quartz veins also have the highest indium contents: Fe-sphalerite (100-25000 ppm), chalcopyrite (up to 1000 ppm), stannite (up to 60000 ppm). 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 433 ppm with average values of 56 - 65 ppm. 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 oreforming processes doubled indium resources of deposits being the main factors in the formation of high grade indium mineralization. | |
653 | |a индий | ||
653 | |a Дальний Восток | ||
653 | |a касситерит | ||
655 | 4 | |a статьи в журналах |9 879358 | |
700 | 1 | |a Pavlova, G. G. |9 440185 | |
700 | 1 | |a Borisenko, A. S. |9 440186 | |
700 | 1 | |a Vladimirov, Alexander G. |9 99847 | |
700 | 1 | |a Seifert, Th. |9 440187 | |
700 | 1 | |a Phan, Luu Anh |9 440188 | |
700 | 1 | |a Palessky, S. V. |9 440189 | |
710 | 2 | |a Томский государственный университет |b Геолого-географический факультет |b Научные подразделения ГГФ |9 118729 | |
773 | 0 | |t Ore geology reviews |d 2015 |g Vol. 66. P. 99-113 |x 0169-1368 | |
852 | 4 | |a RU-ToGU | |
856 | 7 | |u http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000529051 | |
856 | |y Перейти в каталог НБ ТГУ |u https://koha.lib.tsu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=390194 | ||
908 | |a статья | ||
999 | |c 390194 |d 390194 |