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DOI10.1016/j.jog.2019.101690
Kinematic evolution of the West Burma block during and after India-Asia collision revealed by paleomagnetism
Li, Zhenyu; Ding, Lin; Zaw, Than; Wang, Houqi; Cai, Fulong; Yao, Wei; Xiong, Zhongyu; Sein, Kyaing; Yue, Yahui
通讯作者Ding, L (通讯作者)
发表日期2020
ISSN0264-3707
卷号134
英文摘要The magnitude and timing of deformation in the form of vertical-axis rotation in the eastern Tibetan Plateau and Southeast Asia during the Cenozoic period are the key to understanding the India-Asia collision and subsequent geological processes. Our new paleomagnetic and geochronological data from Myanmar show that the characteristic remanent magnetization (ChRM) mean directions of sedimentary tuffaceous layers (31 effective specimens) and rhyolites (11 paleomagnetic site-mean directions), which formed at similar to 64.4 Ma and similar to 26.6 Ma, were D +/- Delta D/I +/- Delta I = 50.8 degrees +/- 11.0 degrees/33.1 +/- 9.2 degrees with alpha(95) = 9.2 degrees and D +/- Delta D/I +/- Delta I = 356.8 degrees +/- 6.5 degrees/16.9 degrees +/- 6.2 degrees with alpha 95 = 6.2 degrees, respectively. These data indicate that the West Burma Block (WBB) has experienced a significant clockwise rotation of 38.3 degrees +/- 6.9 degrees since similar to 64.4 Ma and a later counterclockwise rotation of 14.6 +/- 4.2 degrees since similar to 26.6 Ma with respect to stable Asia. The clockwise rotation of similar to 40 degrees of the WBB since 64.4 Ma (early Paleocene) with respect to stable Asia is attributable to the India-Asia collision, and the later counterclockwise rotation of 14.6 degrees +/- 4.2 degrees since 26.6 Ma (late Oligocene) is attributable to the dextral-slip faulting activity of the Sagaing Fault. These paleomagnetic analyses, combined with previously published geological research in SE Asia, are substantially consistent with the predictions of the extrusion model for the SE Asia realm.
关键词CLOCKWISE ROTATIONCRETACEOUS ROCKSSOUTHERN TIBETARC BASINFOLD TESTDEFORMATIONCHINAHISTORYTECTONICSEXTRUSION
英文关键词West Burma block; Kinematic evolution; Vertical-Axis rotation; Paleomagnetism; Zircon U-Pb dating
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000519667600006
来源期刊JOURNAL OF GEODYNAMICS
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/259739
推荐引用方式
GB/T 7714
Li, Zhenyu,Ding, Lin,Zaw, Than,et al. Kinematic evolution of the West Burma block during and after India-Asia collision revealed by paleomagnetism[J]. 中国科学院青藏高原研究所,2020,134.
APA Li, Zhenyu.,Ding, Lin.,Zaw, Than.,Wang, Houqi.,Cai, Fulong.,...&Yue, Yahui.(2020).Kinematic evolution of the West Burma block during and after India-Asia collision revealed by paleomagnetism.JOURNAL OF GEODYNAMICS,134.
MLA Li, Zhenyu,et al."Kinematic evolution of the West Burma block during and after India-Asia collision revealed by paleomagnetism".JOURNAL OF GEODYNAMICS 134(2020).
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