Crustal velocity structure and earthquake processes of Garhwal-Kumaun Himalaya: Constraints from regional waveform inversion and array beam modeling

被引:37
|
作者
Negi, Sanjay S. [1 ]
Paul, Ajay [1 ]
Cesca, Simone [2 ]
Kamal [3 ]
Kriegerowski, Marius [4 ]
Mahesh, P. [5 ]
Gupta, Sandeep [6 ]
机构
[1] Wadia Inst Himalayan Geol, Dehra Dun 248001, India
[2] GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany
[3] Indian Inst Technol, Dept Earth Sci, Roorkee, Uttar Pradesh, India
[4] Univ Potsdam, Inst Earth & Environm Sci, Potsdam, Germany
[5] Inst Seismol Res, Gandhinagar 382009, Gujarat, India
[6] Natl Geophys Res Inst, Hyderabad, Andhra Pradesh, India
关键词
Travel-time inversion; Moment tensor inversion; Green's functions; Critical taper wedge; Lesser Himalayan Duplex; Out-of-sequence thrust; MOMENT TENSOR INVERSION; FAULT PLANE SOLUTIONS; MAIN CENTRAL THRUST; LESSER HIMALAYA; SEISMIC CYCLE; SEISMOTECTONIC MODEL; NORTHWEST HIMALAYA; TECTONIC EVOLUTION; CHAMOLI EARTHQUAKE; SURFACE RUPTURE;
D O I
10.1016/j.tecto.2017.05.007
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In order to understand present day earthquake kinematics at the Indian plate boundary, we analyse seismic broadband data recorded between 2007 and 2015 by the regional network in the Garhwal-Kumaun region, northwest Himalaya. We first estimate a local 1-D velocity model for the computation of reliable Green's functions, based on 2837 P-wave and 2680 S-wave arrivals from 251 well located earthquakes. The resulting 1-D crustal structure yields a 4-layer velocity model down to the depths of 20 km. A fifth homogeneous layer extends down to 46 km, constraining the Moho using travel-time distance curve method. We then employ a multistep moment tensor (MT) inversion algorithm to infer seismic moment tensors of 11 moderate earthquakes with M-w magnitude in the range 4.05.0. The method provides a fast MT inversion for future monitoring of local seismicity, since Green's functions database has been prepared. To further support the moment tensor solutions, we additionally model P phase beams at seismic arrays at teleseismic distances. The MT inversion result reveals the presence of dominant thrust fault kinematics persisting along the Himalayan belt. Shallow low and high angle thrust faulting is the dominating mechanism in the Garhwal-Kumaun Himalaya. The centroid depths for these moderate earthquakes are shallow between 1 and 12 km. The beam modeling result confirm hypocentral depth estimates between 1 and 7 km. The updated seismicity, constrained source mechanism and depth results indicate typical setting of duplexes above the mid crustal ramp where slip is confirmed along out-of-sequence thrusting. The involvement of Tons thrust sheet in out-of-sequence thrusting indicate Tons thrust to be the principal active thrust at shallow depth in the Himalayan region. Our results thus support the critical taper wedge theory, where we infer the microseismicity cluster as a result of intense activity within the Lesser Himalayan Duplex (LHD) system. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:45 / 63
页数:19
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