Geological, Mineralogical, and Geochemical Features of the Ugakhan Gold Ore Deposit of the Sukhoi Log Type (Baikal-Patom Belt)

被引:6
作者
Budyak, A. E. [1 ,2 ]
Chugaev, A. V. [3 ]
Tarasovaa, Yu. I. [1 ,2 ]
Goryachev, N. A. [1 ,4 ]
Blinov, A. V. [1 ,2 ]
Abramova, V. D. [3 ]
Rassokhina, I. V. [3 ]
Reutskiy, V. N. [5 ]
Ignatiev, A. V. [6 ]
Velivetskaya, T. A. [6 ]
Vanin, V. A. [7 ]
机构
[1] Russian Acad Sci, Vinogradov Inst Geochem, Siberian Branch, Ul Favorskogo 1a, Irkutsk 664033, Russia
[2] Irkutsk Natl Res Tech Univ, Ul Lermontova 83, Irkutsk 664074, Russia
[3] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Staromonetnyi Per 35, Moscow 119017, Russia
[4] Russian Acad Sci, Nrth East Interdisciplinary Sci Res Inst N A N A S, Far East Branch, ul Portovaya 16, Magadan 685000, Russia
[5] Russian Acad Sci, VS Sobolev Inst Geol & Mineral, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia
[6] Russian Acad Sci, Far East Branch, Far East Geol Inst, Pr 100 Letiya Vladivostoka 159, Vladivostok 690022, Russia
[7] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Ul Lermontova 128, Irkutsk 664033, Russia
基金
俄罗斯科学基金会;
关键词
Neoproterozoic; black-shale strata; Ugakhan deposit; Sukhoi Log type; Lena gold ore province; Baikal-Patom belt; NORTHERN TRANSBAIKALIA EVIDENCE; MC-ICP-MS; LEAD-ISOTOPE; METASEDIMENTARY ROCKS; OROGENIC GOLD; EASTERN TRANSBAIKALIA; PB-PB; SM-ND; MINERALIZATION; EVOLUTION;
D O I
10.2113/RGG20234606
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Ugakhan gold ore deposit is located within the Lena gold ore province, the largest one in Russia. It belongs to the group of deposits of the Sukhoi Log genetic type. We present results of petrological, mineralogical, and isotope-geochemical study of gold mineralization at the deposit. A scheme of the sequence of mineral formation at the deposit has been developed, which includes five stages: (1) the early (syndiagenetic) stage, when framboid pyrite I enriched in Au, Ni, Co, and As formed; 2) the stage of catagenesis of ore -bearing sediments, with recrystallization of early pyrite I and crystallization of pyrite II, also with elevated Au, Ni, Co, and As contents; (3) the stage of progressive metamorphism, with the formation of ore pyrrhotite from a water-CO2 fluid with a high content of H2S; (4) the ore formation stage, marked by an assemblage of pyrite III, galena, sphalerite, chalcopyrite, and native gold at the deposit, which was synchronous with regressive metamorphism in the region; (5) crystallization of post -ore euhedral coarse -grained pyrite IV. The geochemical and isotope (delta 34S and Pb-Pb) data rule out the input of mineral -forming components from an additional (external) source during the hydrothermal-metasomatic transformation of ore -bearing rocks. The delta 34S values in the early morphotypes of pyrite in the deposit ores vary from +5.7 to +9.1%o and are close to the delta 34S values of the barren rocks of the Buzhuikhta Formation (+4.2 to +16.4%o). The Pb-Pb isotope characteristics and regularities of variations in Pb isotope composition established for gold mineralization indicate a predominant inflow of lead from Neoproterozoic metasedimentary strata. The mineral and geochemical specifics of the Ugakhan deposit are consistent with the concept of the metamorphic origin of gold deposits of the Sukhoi Log type, which confirms that the rocks of the Buzhuikhta Formation are promising for new gold ore objects.
引用
收藏
页码:404 / 424
页数:21
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