CLC number: P58; P59
On-line Access: 2024-08-27
Received: 2023-10-17
Revision Accepted: 2024-05-08
Crosschecked: 0000-00-00
Cited: 18
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Yang Shu-Feng, Li Zi-Long, Chen Han-Lin, Chen Wen, Yu Xing. 40Ar-39Ar dating of basalts from Tarim Basin, NW China and its implication to a Permian thermal tectonic event[J]. Journal of Zhejiang University Science A, 2006, 7(101): 320-324.
@article{title="40Ar-39Ar dating of basalts from Tarim Basin, NW China and its implication to a Permian thermal tectonic event",
author="Yang Shu-Feng, Li Zi-Long, Chen Han-Lin, Chen Wen, Yu Xing",
journal="Journal of Zhejiang University Science A",
volume="7",
number="101",
pages="320-324",
year="2006",
publisher="Zhejiang University Press & Springer",
doi="10.1631/jzus.2006.AS0320"
}
%0 Journal Article
%T 40Ar-39Ar dating of basalts from Tarim Basin, NW China and its implication to a Permian thermal tectonic event
%A Yang Shu-Feng
%A Li Zi-Long
%A Chen Han-Lin
%A Chen Wen
%A Yu Xing
%J Journal of Zhejiang University SCIENCE A
%V 7
%N 101
%P 320-324
%@ 1673-565X
%D 2006
%I Zhejiang University Press & Springer
%DOI 10.1631/jzus.2006.AS0320
TY - JOUR
T1 - 40Ar-39Ar dating of basalts from Tarim Basin, NW China and its implication to a Permian thermal tectonic event
A1 - Yang Shu-Feng
A1 - Li Zi-Long
A1 - Chen Han-Lin
A1 - Chen Wen
A1 - Yu Xing
J0 - Journal of Zhejiang University Science A
VL - 7
IS - 101
SP - 320
EP - 324
%@ 1673-565X
Y1 - 2006
PB - Zhejiang University Press & Springer
ER -
DOI - 10.1631/jzus.2006.AS0320
Abstract: This paper reports 40Ar-39Ar ages of northwestern China’s tarim Basin Permian basalts. 40Ar-39Ar age dating for basaltic samples from the Yingan section, Keping area and Damusi section of the southwestern part of tarim Basin yields plateau ages of (281.8±4.2) Ma and a weighted mean value of (290.1±3.5) Ma respectively. This study combined with previous data indicates that the basaltic rocks from the studied area formed during 282~290 Ma. 40Ar-39Ar age dating from the basalts addresses a tectonothermal event in the tarim Basin that occurred during the Early Permian of 278~290 Ma.
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