New data on the age of ore formation in the unique Katugin rare-metal deposit (Aldan Shield)

被引：28

作者：

Kotov, A. B. ^{[1
]}

Vladykin, N. V. ^{[2
]}

Larin, A. M. ^{[1
]}

Gladkochub, D. P. ^{[3
]}

Salnikova, E. B. ^{[1
]}

Sklyarov, E. V. ^{[3
,4
]}

Tolmacheva, E. V. ^{[1
]}

Donskaya, T. V. ^{[3
]}

Velikoslavinsky, S. D. ^{[1
]}

Yakovleva, S. Z. ^{[1
]}

机构：

[1] Russian Acad Sci, Inst Precambrian Geol & Geochronol, St Petersburg, Russia

[2] Russian Acad Sci, Inst Geochem, Siberian Branch, Irkutsk 664003, Russia

[3] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664003, Russia

[4] Far East Fed Univ, Vladivostok, Russia

来源：

DOKLADY EARTH SCIENCES | 2015年 / 463卷 / 01期

基金：

俄罗斯科学基金会;

关键词：

PB ZIRCON AGES;

D O I：

10.1134/S1028334X15070107

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Katugin composite rare metal (Ta, Nb, Zr, Y, and REE) deposit is one of the largest Precambrian rare metal deposits associated with alkalic granite in the world [ 1]. It is located at the southern margin of the Chara- Olyokma block of the Aldan Shield in the immediate vicinity of the southern boundary of the Stanovoi Structural Suture, which separates this block from the Selenga- Stanovoi superterrane of the Cen tral Asian Fold Belt (Fig. 1). The deposit is associated with two small (3 and 18 km2) bodies of alkalic granites of the Katugin Complex, which are confined within the limits of the sublatitudinal Kalakan Tectonic Zone stretching along the southern marginal part of the Palaeoproterozoic Kodar- Udokan depression. The latter is composed mainly of metasiliciclastics of the Udokan Group. The geological structure of the Katugin deposit has been described earlier [3, 4, and others].

引用

页码：663 / 667

页数：5

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