The Ryabinovoe Porphyry Cu-Au Deposit (Southern Yakutia): Geology, Wallrock Alteration, Noble Gases Isotope Systematics and Isotopic Dating of Mineralization Processes

被引:0
|
作者
Shatova, N. V. [1 ]
Molchanov, A. V. [1 ]
Terekhov, A. V. [1 ]
Shatov, V. V. [1 ]
Petrov, O. V. [1 ]
Sergeev, S. A. [1 ]
Prasolov, E. M. [1 ]
Dvornik, G. P. [2 ]
Leontev, V. I. [1 ,3 ]
机构
[1] AP Karpinsky Russian Geol Res Inst, St Petersburg 199106, Russia
[2] Russian Acad Sci, AN Zavaritsky Inst Geol & Geochem, Ural Branch, Ekaterinburg 620144, Russia
[3] St Petersburg Min Univ, St Petersburg 199106, Russia
关键词
isotopic geochemistry of noble gases; geochronology; wallrock alteration; ore-forming processes; Ryabinovoe porphyry Cu-Au Deposit; Southern Yakutia; CENTRAL ALDAN; HYDROTHERMAL ALTERATION; LORRAINE DEPOSIT; BRITISH-COLUMBIA; OXYGEN; HYDROGEN; GENESIS; ZONE;
D O I
10.1134/S1075701524010045
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In the territory of the Ryabinovoe porphyry copper-gold deposit, ore mineralization is confined to multi-stage metasomatism fields, which were formed in two stages. At the first, pre-ore stage, high-temperature potassium-sodium metasomatites (aegirine feldspathites) were formed, at the second stage, medium-low-temperature wallrock gumbeites in the form of two facies varieties: carbonate-sericite-muscovite-orthoclase and quartz-carbonate-barite-adular varieties. Results of isotope studies (U-Pb, Rb-Sr, Re-Os, Ar-40/Ar-36, He-3/He-4, Ne-20) of the aforementioned metasomatites and ore mineralization are discussed in the paper.
引用
收藏
页码:120 / 141
页数:22
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