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    • Keywords


      Indian Plate; Aravalli Craton; lineaments; epicenters; GPS.

    • Abstract


      We report site motion of a permanent GPS site at Udaipur (udai), Rajasthan on the Udaipur block of Aravalli Craton. The GPS measurements of 2007–2011 suggest that the site moves at a rate of about 49 mm/year towards northeast. As the site motion is consistent with the predicted plate motion using the estimated euler pole of rotation for the Indian Plate, it implies that there is insignificant internal deformation/strain in the region. Such a deformation is consistent with very low seismic activity in the region. The epicenters of the infrequent low magnitude earthquakes are located on the Precambrian lineaments on the west of Udaipur Block, and on the NW–SE striking younger lineament in the south of the block.

    • Author Affiliations


      Harsh Bhu1 Ritesh Purohit2 Joga Ram2 Pankaj Sharma2 S R Jakhar3

      1. Department of Geology, ML Sukhadia University, Udaipur 313 001, India.
      2. Department of Geology, Government College, Sirohi 307 001, India.
      3. Department of Geology, JNV University, Jodhpur 342 001, India.
    • Dates

  • Journal of Earth System Science | News

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      Posted on July 25, 2019

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