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DOI | 10.1007/s00024-018-1872-3 |
Contemporary Crustal Deformation Within the Pamir Plateau Constrained by Geodetic Observations and Focal Mechanism Solutions | |
Pan, Zhengyang; He, Jiankun; Li, Jun | |
通讯作者 | Pan, ZY (通讯作者) |
发表日期 | 2018 |
ISSN | 0033-4553 |
EISSN | 1420-9136 |
起始页码 | 3463 |
结束页码 | 3484 |
卷号 | 175期号:10 |
英文摘要 | We used an updated data set of 192 GPS-derived surface velocities and 393 earthquake focal mechanisms (Mw > 3.0, hypocenter depths < 30 km) to evaluate the spatial variations in the surface strain rate and crustal stress regime throughout the Pamir Plateau and its surrounding regions. The strain rate field was estimated using the spline in tension approach that solves for the surface velocity in a rectangular grid and the stress field was predicted from focal mechanism solutions using the damped regionalscale stress inversion (DRSSI) method of Hardebeck and Michael (Journal of Geophysical Research, https://doi. org/10.1029/ 2005jb004144, 2006). The results show that the crustal stress field around the Pamir Plateau is predominantly characterized by NNW-SSE compression and E-W extension, which is consistent with the principal orientations of the two-dimensional surface strain rate tensor. This agreement supports the notion that the Pamir and southwestern Tien Shan are uniformly strained blocks. In particular, the fan-shaped rotational pattern between Shmax and the strain rate from the western Pamir to the Tajik Basin shows that the counterclockwise rotation of the Shmax orientation is associated with vertical deformation, which is consistent with the idea of Schurr et al. (Tectonics 33(8): 2014TC003576, 2014) concerning the gravitational collapse and westward extrusion of the crust in the western Pamir. We propose that such a stress-strain pattern, dominated by NNW-ESE oriented compression and E-W trending extension, originated from a combination of the northward push of the Indian continent and the southward subduction of the Tien Shan. |
关键词 | BAND REGIONAL SEISMOGRAMSFAULT PLANE SOLUTIONSSOUTHERN TIEN-SHANSTRAIN-RATE FIELDSSTRESS-FIELDKARAKORAM FAULTWENCHUAN EARTHQUAKETARIM BASINNORTHWESTERN CHINAGPS OBSERVATIONS |
英文关键词 | Focal mechanism; geodetic strain; active deformation; Pamir Plateau; India-Eurasia collision |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000447266800006 |
来源期刊 | PURE AND APPLIED GEOPHYSICS |
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/259188 |
推荐引用方式 GB/T 7714 | Pan, Zhengyang,He, Jiankun,Li, Jun. Contemporary Crustal Deformation Within the Pamir Plateau Constrained by Geodetic Observations and Focal Mechanism Solutions[J]. 中国科学院青藏高原研究所,2018,175(10). |
APA | Pan, Zhengyang,He, Jiankun,&Li, Jun.(2018).Contemporary Crustal Deformation Within the Pamir Plateau Constrained by Geodetic Observations and Focal Mechanism Solutions.PURE AND APPLIED GEOPHYSICS,175(10). |
MLA | Pan, Zhengyang,et al."Contemporary Crustal Deformation Within the Pamir Plateau Constrained by Geodetic Observations and Focal Mechanism Solutions".PURE AND APPLIED GEOPHYSICS 175.10(2018). |
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