Structure, Mineralogical, and Geochemical Features and Formation Conditions of Ore Veins in the Mo Porphyry Shakhtama Deposit (Eastern Transbaikalia)

被引:1
|
作者
Yurgenson, G. A. [1 ]
Kiseleva, G. D. [2 ]
Dolomanova-Topol, A. A. [2 ]
Kovalenker, V. A. [2 ]
Petrov, V. A. [2 ]
Yazykova, Yu. I. [2 ]
Levitskaya, L. A. [2 ]
Trubkin, N. V. [2 ]
Taskaev, V. I. [2 ]
Karimova, O. B. [2 ]
机构
[1] Russian Acad Sci, Inst Nat Resources Ecol & Cryol, Siberian Branch, Chita 672002, Russia
[2] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia
关键词
Shakhtama Mo deposit; vein structure; mineral zonality; typomorphic features of minerals; svanbergite; fluid inclusions; formation conditions; MOLYBDENITE; EVOLUTION; REGION;
D O I
10.1134/S1075701523070243
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The results of a comprehensive detailed study of the vein structure, mineral zoning of veins, and mineral typomorphism of the Shakhtama deposit obtained on the basis of new samples from poorly studied horizons are given. The results obtained show that the Mo resources of the deposit are far from being exhausted, and the typomorphic features of ore minerals indicate that base metal mineralization associated with Au (Ag), also continues to a depth, along with Mo. The presence of rare Sr mineral, svanbergite, in the Shakhtama deposit and the typomorphic properties of ore minerals testify in favor of the near-surface origin of the exposed mineralization. The succession of mineral formation has been established. Based on the study of ore and metasomatic zonality, fluid inclusions and isotopic data, as well as the composition of structural impurities in molybdenite, conclusions were made of the formation conditions of ore mineralization in a porphyry ore-forming system.
引用
收藏
页码:S153 / S188
页数:36
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