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India plate angular velocity and contemporary deformation rates from continuous GPS measurements from 1996 to 2015

机译:1996年至2015年通过连续GPS测量获得的印度板块角速度和当代变形率

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摘要

We estimate a new angular velocity for the India plate and contemporary deformation rates in the plate interior and along its seismically active margins from Global Positioning System (GPS) measurements from 1996 to 2015 at 70 continuous and 3 episodic stations. A new India-ITRF2008 angular velocity is estimated from 30 GPS sites, which include stations from western and eastern regions of the plate interior that were unrepresented or only sparsely sampled in previous studies. Our newly estimated India-ITRF2008 Euler pole is located significantly closer to the plate with ~3% higher angular velocity than all previous estimates and thus predicts more rapid variations in rates and directions along the plate boundaries. The 30 India plate GPS site velocities are well fit by the new angular velocity, with north and east RMS misfits of only 0.8 and 0.9 mm/yr, respectively. India fixed velocities suggest an approximate of 1–2 mm/yr intra-plate deformation that might be concentrated along regional dislocations, faults in Peninsular India, Kachchh and Indo-Gangetic plain. Relative to our newly-defined India plate frame of reference, the newly estimated velocities for 43 other GPS sites along the plate margins give insights into active deformation along India’s seismically active northern and eastern boundaries.
机译:我们根据1996年至2015年全球70个连续和3个突发性站点的全球定位系统(GPS)测量,估计了印度板块的新角速度和板块内部及其沿地震活动边缘的现代变形率。从30个GPS站点估计了一个新的India-ITRF2008角速度,其中包括来自板块内部的西部和东部地区的站点,这些站点在以前的研究中没有或仅被稀疏地采样。我们新近估算的India-ITRF2008欧拉极点比板块更近,角速度比以前的估计高出约3%,因此可以预测沿板块边界的速率和方向的变化更快。新的角速度很好地适应了30个印度板块GPS站点速度,北和东RMS失配分别仅为0.8和0.9 mm / yr。印度的固定速度表明板块内部变形大约为1-2 mm / yr,这可能集中在区域性位错,印度半岛,Kachchh和印度恒河平原的断层上。相对于我们新定义的印度板块参考系,板块边缘沿其他43个GPS站点的最新估算速度可以洞悉印度北部和东部地震活跃边界的活动变形。

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