Climate Change Data Portal
DOI | 10.1016/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 |
ISSN | 0264-3707 |
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). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。