New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan)

被引：7
|
作者：
Khudoley, A. K. [1 ]
Alexeiev, D. V. [2 ]
DuFrane, S. A. [3 ]
Degtyarev, K. E. [2 ]
Letnikova, E. F. [4 ]
机构：
[1] St Petersburg State Univ, Inst Earth Sci, St Petersburg 199034, Russia
[2] Russian Acad Sci, Geol Inst, Moscow 119017, Russia
[3] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB, Canada
[4] Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk 630090, Russia
来源：
DOKLADY EARTH SCIENCES | 2018年 / 479卷 / 01期
基金：
俄罗斯科学基金会; 俄罗斯基础研究基金会;
关键词：
SHAN;
D O I：
10.1134/S1028334X18030182
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
U-Pb dating of detrital zircon from the Kokdjot Group and Bolshekaroi Formation (Malyi Karatau) yielded for all the samples age clusters at about 800-805, 855-890, 1980-2100, and 2440-2470 Ma. The Kolmogorov-Smirnov test suggests they have identical provenance sources. The Kokdjot Group and Bolshekaroi Formation ages are presumably Neoproterozoic, not older than 800 Ma, though a somewhat younger age (not older 770 Ma) cannot be ruled out.
引用
收藏
页码：316 / 319
页数：4
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