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...

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Bibliographic Details
Published in:Ore geology reviews Vol. 66. P. 99-113
Corporate Author: Томский государственный университет Геолого-географический факультет Научные подразделения ГГФ
Other Authors: Pavlova, G. G., Borisenko, A. S., Vladimirov, Alexander G., Seifert, Th, Phan, Luu Anh, Palessky, S. V.
Format: Article
Language:English
Subjects:
Online Access:http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000529051
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039 9 |a 201812021547  |c 201604060757  |d cat202  |c 201604041622  |d VLOAD  |y 201604041613  |z Александр Эльверович Гилязов 
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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. 
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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 
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