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      Permanent link:
      https://www.ias.ac.in/article/fulltext/jess/117/03/0181-0188

    • Keywords

       

      Active fault; trench investigation; Kachchh; Katrol Hill Fault.

    • Abstract

       

      Several new active fault traces were identified along Katrol Hill Fault (KHF).A new fault (named as Bhuj Fault,BF)that extends into the Bhuj Plain was also identified.These fault traces were identified based on satellite photo interpretation and field survey.Trenches were excavated to identify the paleoseismic events,pattern of faulting and the nature of deformation.New active fault traces were recognized about 1 km north of the topographic boundary between the Katrol Hill and the plain area.The fault exposure along the left bank of Khari River with 10 m wide shear zone in the Mesozoic rocks and showing displacement of the overlying Quaternary deposits is indicative of continued tectonic activity along the ancient fault.The E-W trending active fault traces along the KHF in the western part changes to NE-SW or ENE-WSW near Wandhay village.

      Trenching survey across a low scarp near Wandhay village reveals three major fault strands F1, F2,and F3.These fault strands displaced the older terrace deposits comprising Sand,Silt and Gravel units along with overlying younger deposits from units 1 to 5 made of gravel,sand and silt. Stratigraphic relationship indicates at least three large magnitude earthquakes along KHF during Late Holocene or recent historic past.

    • Author Affiliations

       

      Michio Morino1 Javed N Malik2 Prashant Mishra2 Chandrashekhar Bhuiyan2 Fumio Kaneko1

      1. OYO International Corporation, Rokubancho Kyodo Bldg. 2F, 6 Rokubancho, Chiyoda-ku, Tokyo, Japan 102-0085.
      2. Department of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur 208 016, India.
    • Dates

       
  • Journal of Earth System Science | News

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