Tin-bearing magmatic complexes of the Russian Far East

被引：0
|
作者：
Gonevchuk, VG [1 ]
Semenjak, BI [1 ]
Khanchuk, AI [1 ]
Gonevchuk, GA [1 ]
机构：
[1] Russian Acad Sci, Far E Geol Inst, Far E Branch, Vladivostok 690022, Russia
来源：
MINERAL DEPOSITS: PROCESSES TO PROCESSING, VOLS 1 AND 2 | 1999年
关键词：
D O I：
暂无
中图分类号：
P57 [矿物学];
学科分类号：
070901 ;
摘要：
The tin mineralization of the Russian Far East is present in different mineral successions and is related with different types of granites which are located in different terranes. In Paleozoic terranes (Bureya, Khanka and Badzhal) granites of S-type series transitive to A- or I-type series, and cassiterite-quartz mineralization prevail. In the Zhuravlevka turbidite terrane of Mesozoic age prevail I-type granitoids and cassiterite-silicate-sulphide mineralization.
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页码：357 / 359
页数：3
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