The Age of Transformation of Rare-Metal Alkaline Granites of the Katugin Massif (Aldan Shield)

被引：2

作者：

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

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

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

Sklyarov, E. V. ^{[2
,3
]}

Gladkochub, D. P. ^{[2
]}

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

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

Donskaya, T. V. ^{[2
]}

Vladykin, N. V. ^{[4
]}

Radomskaya, T. A. ^{[4
]}

机构：

[1] Russian Acad Sci, Inst Precambrian Geol, St Petersburg 199034, Russia

[2] Russian Acad Sci, Siberian Branch, Inst Earths Crust, Irkutsk 664033, Russia

[3] Far East Fed Univ, Vladivostok 690000, Russia

[4] Russian Acad Sci, Vinogradov Inst Geochem, Siberian Branch, Irkutsk 650033, Russia

来源：

DOKLADY EARTH SCIENCES | 2018年 / 478卷 / 01期

基金：

俄罗斯科学基金会;

关键词：

DEPOSIT; COMPLEXES; SETTINGS;

D O I：

10.1134/S1028334X18010026

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The U-Pb (ID TIMS) geochronological studies of single zircon grains and their fragments have made it possible to establish that rare-metal alkaline granites of the Katugin massif (2055 +/- 7aEuro'2066 +/- 6 Ma) underwent high-temperature transformations at age levels of 1921 +/- 5 and 1876 +/- 7 Ma.

引用

页码：1 / 6

页数：6

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