Kashmir Basin Fault and its tectonic significance in NW Himalaya, Jammu and Kashmir, India
详细信息    查看全文
  • 作者:A. A. Shah
  • 关键词:NW Himalaya ; Kashmir Basin Fault ; Out ; of ; sequence thrusting ; Jammu and Kashmir
  • 刊名:International Journal of Earth Sciences
  • 出版年:2015
  • 出版时间:October 2015
  • 年:2015
  • 卷:104
  • 期:7
  • 页码:1901-1906
  • 全文大小:6,165 KB
  • 参考文献:Ader T, Avouac Jean-Philippe, Liu-Zeng Jing et al (2012) Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: implications for seismic hazard. J Geophy Res 117:B04403
    Ahmad S, Bhat MI, Madden C et al (2013) Geomorphic analysis reveals active tectonic deformation on the eastern flank of the PirPanjal Range, Kashmir Valley India. Arab J Geo 6:1-1
    Ambraseys N, Douglas J (2004) Magnitude calibration of north Indian earthquakes. Geophys J Int 159:165-06CrossRef
    Ambraseys N, Jackson D (2003) A note on early earthquakes in northern India and southern Tibet. Curr Sci 84:570-82
    Armbruster J, Seeber L, Jacob KH (1978) The northwestern termination of the Himalayan mountain front: active tectonics from microearthquakes. J Geophys Res 83:269-81CrossRef
    Avouac JP, Ayoub F, Leprince S et al (2006) The 2005, Mw 7.6 Kashmir earthquake: sub-pixel correlation of ASTER images and seismic waveforms analysis. Earth Planet Sci Lett 249:514-28CrossRef
    Banerjee P, Bürgmann R (2002) Convergence across the northwest Himalaya from GPS measurements. Geophy Res Lett 29:30-1
    Bashir A, Bhat MI, Bali BS (2009) Historical record of earthquakes in the Kashmir valley. J Himal Geol 30:75-4
    Bhatt DK (1976) Stratigraphical status of Karewa Group of Kashmir, India. J Himal Geol 6:197-08
    Bilham R, Bali BS (2014) A ninth century earthquake-induced landslide and flood in the Kashmir Valley, and earthquake damage to Kashmir’s Medieval temples. B Earthq Eng 12:79-09CrossRef
    Bilham R, Larson K, Freymueller J et al (1997) GPS measurements of present-day convergence across the Nepal Himalaya. Nature 386:61-4CrossRef
    Bilham R, Bali BS, Bhat MI, Hough S (2010) Historical earthquakes in Srinagar, Kashmir: clues from the Shiva temple at Pandrethan. Geol Soc Amer Special Papers 47:107-17CrossRef
    Bollinger L, Sapkota SN, Tapponnier P et al (2014) Estimating the return times of great Himalayan earthquakes in eastern Nepal: evidence from the Patu and Bardibas strands of the Main Frontal Thrust. J Geophys Res Solid Earth 119:7123-163CrossRef
    Burbank DW, Johnson GD (1982) Intermontane-basin development in the past 4 Myr in the north-west Himalaya. Nature 298:432-36CrossRef
    Burbank DW, Johnson GD (1983) The Late Cenozoic chronologic and stratigraphic development of the Kashmir intermontane basin, northwestern Himalaya. Palaeogeogr Palaeoclimatol Palaeoecol 43:205-350CrossRef
    Burbank DW, Raynolds RGH, Johnson GD (1986) Late Cenozoic tectonics and sedimentation in the north-western Himalayan foredeep, II, Eastern limb of the northwest syntaxis and regional synthesis. In: Spec Publ Int Assoc Sedimentol 8:293-30
    Jackson M, Bilham R (1994) GPS measurements across the Nepal Himalaya. Geophys Res Lett 2:1169-172CrossRef
    Kaneda H, Nakata T, Tsutsumi H et al (2008) Surface rupture of the 2005 Kashmir, Pakistan, earthquake, and its active tectonic implications. Bull Seis Soc Amer 98:521-57CrossRef
    Kumahara Y, Jayangondaperumal R (2013) Paleoseismic evidence of a surface rupture along the northwestern Himalayan Frontal Thrust (HFT). Geomorphology 180:47-6CrossRef
    Kumahara Y, Nakata T (2006) Active Faults in the Epicentral Area of the 2005 Pakistan Earthquake. In: Spec Publ Res Cent Reg Geogr Hiroshima Univ 41: 54
    Lave J, Avouac JP (2000) Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal. J Geophys Res 105:5735-770CrossRef
    Malik JN, Sahoo AK, Shah AA et al (2010) Paleoseismic evidence from trench investigation along Hajipur fault, Himalayan Frontal Thrust, NW Himalaya: implications of the faulting pattern on landscape evolution and seismic hazard. J Struct Geol 32:350-61CrossRef
    Malik JN, Shah AA, Naik SP et al (2014) Active fault study along foothill zone of Kumaun Sub-Himalaya: influence on landscape shaping and drainage evolution. Curr Sci 106:229
    Molnar P, Stock JM (2009) Slowing of India’s convergence with Eurasia since 20?Ma and its implications for Tibetan mantle dynamics. Tectonics 28:3CrossRef
    Mukherjee S, Koyi HA, Talbot CJ (2012) Implications of channel flow analogue models for extrusion of the Higher Himalayan Shear Zone with special reference to the out-of-sequence thrusting. Int J Earth Sci 10:253-72CrossRef
    Pandey MR, Tandukar RP, Avouac JP et al (1999) Seismotectonics of Nepal himalayas from a local seismic network. J Asian Earth Sci 17:703-12CrossRef
    Powers PM, Lillie RJ, Yeats RS (1998) Structure and shortening of the Kangra and Dehra Dun reentrants, sub-Himalaya, India. Geol Soc Amer Bull 110:1010-027CrossRef
    Schiffman C, Bali Bikram Singh, Szeliga Walter et al (2013) Seismic slip deficit in the Kashmir Himalaya from GPS observations. Geophys Res Lett 40:5642-645CrossRef
    Shabir A, Bhat MI (2012) Tectonic geomorphology of the Rambiara basin, SW Kashmir Valley reveals emergent = out-of-sequence active fault system. Himal Geol 33:162-72
    Shah AA (201
  • 作者单位:A. A. Shah (1) (2)

    1. Curtin University Sarawak, 98009, Miri, Malaysia
    2. Physical and Geological Sciences Programme, Faculty of Science, Universiti Brunei Darussalam, Bandar Seri Begawan, BE1410, Brunei Darussalam
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geology
    Geophysics and Geodesy
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1437-3262
文摘
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 411:241-52, 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. Keywords NW Himalaya Kashmir Basin Fault Out-of-sequence thrusting Jammu and Kashmir

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700