Abstract
The Kashmir Basin Fault is located in the Jammu and Kashmir region of Kashmir Basin in NW Himalaya, India. It is a classic example of an out-of-sequence thrust faulting and is tectonically active as observed from multiple geological evidences. Its geomorphology, structure and lateral extent indicate significant accommodation of stress since long, which is further supported by the absence of a large earthquake in this region. It seems this fault is actively accommodating some portion of the total India–Eurasia convergence, apart from two well-recognised active structures the Medlicott–Wadia Thrust and the Main Frontal Thrust, which are referred in Vassallo et al. (Earth Planet Sci Lett 411:241–252, 2015). This requires its quantification and inclusion into slip distribution scheme of NW Himalaya. Therefore, it should be explored extensively because this internal out-of-sequence thrust could serve major seismic hazard in KB, repeating a situation similar to Muzaffarabad earthquake of Northern Pakistan in 2005.
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Acknowledgments
I am very thankful to Dr. Seema Sing, Dr. Soumyajit Mukherjee and, Dr. S.S. Bhakuni for a rigorous review of this manuscript, which has greatly improved its contents. I am grateful to Prof. W. Christian Dullo for editorial handling and to Monika Dullo for managing support to the journal. Special thanks to Prof. J.N. Malik (IITK) for his guidance and help throughout the preparation of this manuscript.
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Shah, A.A. Kashmir Basin Fault and its tectonic significance in NW Himalaya, Jammu and Kashmir, India. Int J Earth Sci (Geol Rundsch) 104, 1901–1906 (2015). https://doi.org/10.1007/s00531-015-1183-1
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DOI: https://doi.org/10.1007/s00531-015-1183-1