Age and Stratigraphic Position of Sedimentary Sequences of the Bagrush Mountains (Southern Urals) Based on the Results of U-Pb Dating (LA-ICP-MS) of Detrital Zircons

被引:2
|
作者
Romanyuk, T. V. [1 ]
Kuznetsov, N. B. [2 ,3 ,6 ]
Puchkov, V. N. [4 ]
Sergeeva, N. D. [5 ]
Powerman, V. I. [1 ,6 ]
Gorozhanin, V. M. [5 ]
Gorozhanina, E. N. [5 ]
机构
[1] Russian Acad Sci, Schmidt Inst Phys Earth, Moscow 123995, Russia
[2] Russian Acad Sci, Geol Inst, Moscow 119017, Russia
[3] Gubkin Russian State Univ Oil & Gas, Moscow 119991, Russia
[4] Russian Acad Sci, Ural Branch, Zavaritsky Inst Geol & Geochem, Ekaterinburg 620016, Russia
[5] Russian Acad Sci, Ufa Fed Res Ctr, Inst Geol, Ufa 450077, Russia
[6] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664033, Russia
关键词
Southern Urals; Bagrush Mountains; Riphean; detrital zircons; U-Pb dating; RIPHEAN SANDSTONES;
D O I
10.1134/S1028334X20080188
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In order to determine the provenance and age of terrigenous-carbonate stratified units exposed in the region of Bagrush Mountains, Bashkirian uplift, U-Pb dating of detrital zircons from these units has been carried out. A comparison of the data results with analogous data on five stratigraphic levels within the Riphean section of the Bashkirian uplift has shown that the studied sequence should be, most likely, correlated to the uppermost Lower Riphean or the lowermost Middle Riphean.
引用
收藏
页码:593 / 599
页数:7
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