Formation of Gold Mineralization under Amphibolite Facies Metamorphism: Ykan Deposit (Baikal–Patom Belt)

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
A. E. Budyak, Yu. I. Tarasova, A. V. Chugaev, N. A. Goryachev, T. A. Velivetskaya, A. V. Ignatiev
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引用次数: 0

Abstract

Black shale sequences whose metamorphic grade exceeds the regional greenschist facies are considered by most researchers exclusively as promising for alluvial gold. The paper reports the results of a study of the Ykan deposit, located within the epidote–amphibolite facies zone, and its comparison with previously studied deposits localized in the greenschist-facies alteration zone. It was found that the the main factor of localization of the Ykan gold deposit is its lithological and stratigraphical restriction to the contact between carbonaceous phyllite shales and sandstones of the Aunakit Formation in the hanging wall of the anticline. The ore mineralization of the deposit is represented by a subsequent change of early dia-catagenetic pyrite (py-I, py-II) → metamorphogenic pyrrhotite (po, cpy, asp) → metamorphogenic-metasomatic pyrite–base metal (cpy, asp, py-III, gln, sph, pn, mrc) → postore pyrite (py-IV) assemblages. The ore stage is characterized by the highest possible PT parameters in the early ore metamorphic phase and their decrease at the ore-productive phase. Data on variations in the sulfur and lead isotopic composition indicate that they were transported into the ore fluid from the host metasedimentary sequences of the Aunakit Formation. Comparison of the obtained parameters of the Ykan deposit with the previously studied Sukhoi Log, Golets Vysochaishii, Ugakhan, and Krasnoe deposits confirmed that the Ykan deposit can be attributed to the Sukhoi Log-type deposits.

Abstract Image

闪长岩面变质作用下金矿化的形成:伊坎矿藏(贝加尔-帕托姆带)
摘要 大多数研究人员都认为,变质程度超过区域绿岩面的黑色页岩序列很有可能是砂金矿床。本文报告了对位于闪长岩-闪长岩面带内的 Ykan 矿床的研究结果,并将其与之前研究的位于绿岩-岩相蚀变带内的矿床进行了比较。研究发现,Ykan 金矿床定位的主要因素是其岩性和地层局限于反斜坡悬壁的奥纳基特地层碳质辉绿岩页岩和砂岩之间的接触。该矿床的矿石成矿过程表现为:早期二成因黄铁矿(py-I、py-II)→变质黄铁矿(po、cty、asp)→变质-金属黄铁矿-贱金属(cty、asp、py-III、gunn、ph、pn、mrc)→后生黄铁矿(py-IV)组合的后续变化。矿石阶段的特点是,在早期矿石变质阶段,PT 参数可能最高,而在矿石生产阶段,PT 参数可能降低。硫和铅同位素组成的变化数据表明,它们是从奥纳基特地层的主成岩序列运入矿石流体的。将获得的 Ykan 矿床参数与之前研究的 Sukhoi Log、Golets Vysochaishii、Ugakhan 和 Krasnoe 矿床进行比较后证实,Ykan 矿床可归属于 Sukhoi Log 型矿床。
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来源期刊
Russian Journal of Pacific Geology
Russian Journal of Pacific Geology 地学-地球科学综合
CiteScore
1.30
自引率
37.50%
发文量
34
审稿时长
>12 weeks
期刊介绍: Russian Journal of Pacific Geology publishes the results of research on the Earth crust and mantle composition and provides articles on the geological structure and patterns of distribution of mineral deposits in the Pacific Ocean, marginal seas and continental margins. It discusses the topics of stratigraphy, sedimentology, magmatic activity, and seismicity. The journal deals with the problems of lithosphere plates tectonics, and offers the results of neotectonic, geomorphological, geodesic, environmental and mining studies in the Pacific region. The journal accepts theoretical, methodical and philosophical articles covering general issues of geology, geophysics, geochemistry, geoecology and mining. The journal also publishes critical notes and comments, and reviews.
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