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
收藏
页码：1 / 6
页数：6
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