4.4 Article

Present-day crustal deformation and geodetic strain in the vicinity of Dholavira - Harappan civilization site, Kachchh, western part of the Indian plate

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QUATERNARY INTERNATIONAL
卷 507, 期 -, 页码 324-332

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2018.10.035

关键词

GPS geodesy; Harappan civilization; Static slip; Post-seismic deformation; Strain accumulation; Seismic moment; Indian plate

资金

  1. Department of Science and Technology, Govt of Gujarat and Ministry of Earth Sciences, Govt of India [(Seismo-1/270/AFM/2015)]
  2. NOAA

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To understand the geodynamics in the vicinity of Dholavira, a Harappan Civilization Site (HCS), in Kachchh western India, GPS data from 2009 to 2015 were processed and analyzed. Tectonically, this part of northern Kachchh is in the influence of Island Belt Fault (IBF) and Allah Bund Fault (ABF) and is seismically one of the most active intra-plate regions of India. The motion with respect to Indian plate is used for the estimation of deformation and strain rate while fault associated slip rate has been estimated by inverse modeling of observed site motions. The analysis reveals that the ABF deforms with an average rate of 1.8 mm/yr. However, the segmented IBF has a maximum deformation rate of 2.9 mm/yr towards the Pachham Island and minimum towards the Khadir Island. The computation discloses a maximum seismic moment (M-0) of 2.1 x 10(24) dyne-cm in this part which corresponds to an earthquake of approximate to Mw 6.0. The calculated maximum strain of 0.04 micro-strain/year is low but significant in the intra-plate region. The postseismic deformation, after the Mw 7.7, 2001 Bhuj earthquake is estimated to be low in this part. The reverse along with strike-slip motion of faults builds up stress in the area and accumulating more strain.

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