One dimensional regional shear velocity structure from joint inversion of fundamental mode group velocity  dispersion measurements of Love and Rayleigh waves-application to the Uttarakhand Himalaya

Author:

GUPTA ABHISHEK KUMAR1,Mandal Prantik2,Srina D.2,Tiwari Anil1,Sain Kalachand3,Paul Ajay3

Affiliation:

1. WIHG: Wadia Institute of Himalayan Geology

2. NGRI: National Geophysical Research Institute CSIR

3. Wadia Institute of Himalayan Geology

Abstract

Abstract Between 2017 and 2019, the CSIR-NGRI, Hyderabad, Telangana, established a broad-band seismic-network with fifty-five 3-component bb seismometers in the Himalayan region of Uttarakhand, India. Out of 55 three component broadband seismic (BBS) networks, we chose 17 for the present study. Using digital waveform data from twenty-one (21) regional Indian earthquakes of Mw 5.0-6.2 that were recorded in the 17 broadband seismometer, we compute fundamental mode group-velocity dispersion (FMGVD) characteristics of surface waves (love and Rayleigh waves) and the average one-dimensional regional shear-wave velocity (Vs) structure of the Uttarakhand Himalayan region. First, we compute FMGVD curves for Love waves (6-73sec) and Rayleigh waves (at 6.55-73 sec) period and then, we finally invert these dispersion curves to compute the final average one dimensional regional crustal & sub-crustal shear-wave velocity (Vs) structure below the Uttarakhand Himalaya. Our best model in Uttarakhand Himalayan region, India, reveals the 8-layered crust with a mid-crustal low velocity layer (MC-LVL) (approximately a drop of 1.5–2.3% in Vs) between 8 and 20 km depth in the proximity of MCT (Main Central Thrust). In the upper crustal part (0–20 km depths), our modelling suggests shear velocities (Vs) varies from 3.1–3.9 km/sec while shear velocities (Vs) in the lower crustal part (20–45 km depth) are modelled to be varying from 3.7–4.69 km per sec. The Moho-depth is calculated to be 45 km deep below the K-G Himalaya, and the shear-velocity (Vs) in the sub-crustal sector is 4.69 km/sec. Our estimated mid-crustal low velocity layer (MC-LVL) could be linked to the presence of metamorphic fluids in the fractured Main Himalayan Thrust (MHT), resulting from the weakening of the crustal material at the interface between the overriding Eurasian plate and upper -part of the under thrusting Indian plate.

Publisher

Research Square Platform LLC

Reference43 articles.

1. Crustal structure of the Darjeeling-Sikkim Himalaya and southern Tibet;Acton CE;Geophys J lnt,2010

2. Group velocity tomography of the Indo-Eurasian collision zone;Acton CE;J Geophys Res,2010

3. Mountain building, erosion, and the seismic cycle in the Nepal Himalaya;Avouac JP;Adv Geophys,2003

4. Lowered geoflocked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake;Avouac JP;Nat Geosci,2015

5. Moho depth determinations based on spectral ratio analysis of NORSAR long-period P waves;Berteusen KA;Phys of Earth and Planet Int,1977

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3