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首页> 外文期刊>Quaternary International >Hybrid tectonic character of the Kashmir basin: Response to comment on 'Coexistent pre-existing extensional and subsequent compressional tectonic deformation in the Kashmir basin, NW Himalaya (Alam et al., 2017)' by Shah (2017)
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Hybrid tectonic character of the Kashmir basin: Response to comment on 'Coexistent pre-existing extensional and subsequent compressional tectonic deformation in the Kashmir basin, NW Himalaya (Alam et al., 2017)' by Shah (2017)

机译:克什米尔盆地的混合构造特征:回应Shah(2017)发表的评论``喜马拉雅西北部克什米尔盆地既存的伸展性和随后的压缩构造变形(Alam et al。,2017)''

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摘要

In general the genesis of the Kashmir basin is being viewed as a result of compressional tectonics, perhaps because of the reason that the basin is located in India-Eurasia convergence zone. However, there is no work that convincingly demonstrates how existing geomorphic architecture of the Kashmir basin evolved due to thrust tectonics? With answer to many questions Alam et al., (2015) proposed an extensional model for the development of the Kashmir basin. Moreover, based on deformation styles at varied spatial scales Alam et al., (2017) also suggested the co-existence of dominant extensional and relatively feeble compressional deformations within the basin.
机译:总的来说,克什米尔盆地的成因被认为是受压构造的结果,也许是因为该盆地位于印度-欧亚大陆汇合带的原因。但是,没有任何工作能够令人信服地证明克什米尔盆地现有的地貌构造是由于逆冲构造而如何演化的?在回答了许多问题之后,Alam等人(2015年)提出了克什米尔盆地发展的扩展模型。此外,基于不同空间尺度下的变形样式,Alam等人(2017年)还提出了盆地内主要的伸展形变和相对微弱的压缩形变并存。

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  • 来源
    《Quaternary International》 |2018年第ptab期|284-289|共6页
  • 作者单位

    Univ Kashmir, Dept Geog & Reg Dev, Srinagar 190006, Jammu & Kashmir, India;

    Univ Kashmir, Dept Geog & Reg Dev, Srinagar 190006, Jammu & Kashmir, India;

    Kumaun Univ, Ctr Adv Study Geol, Naini Tal 263002, India;

    Nawakadal Sch, Dept Geol, Srinagar 190002, Jammu & Kashmir, India;

    Univ Kashmir, Dept Geog & Reg Dev, Srinagar 190006, Jammu & Kashmir, India;

    Univ Jammu, Dept Remote Sensing & GIS, Jammu 180006, India;

    Univ Kashmir, Dept Geog & Reg Dev, Srinagar 190006, Jammu & Kashmir, India;

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