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首页> 外文期刊>Journal of the Geological Society of India >Neotectonic response of the Godavari and Kaddam rivers in Andhra Pradesh, India: Implications to quaternary reactivation of old fracture system
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Neotectonic response of the Godavari and Kaddam rivers in Andhra Pradesh, India: Implications to quaternary reactivation of old fracture system

机译:印度安得拉邦戈达瓦里河和卡达姆河的新构造响应:对旧裂缝系统的第四纪活化的启示

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摘要

A field and imagery based study at the eastern margin of the Deccan Volcanic Province (DVP), and in the Precambrian terrain of Adilabad and Karimnagar districts of Andhra Pradesh, India display a striking response of the Godavari and Kaddam rivers to Kaddam lineament-fault fracture (KLF) system. Brittle to ductile deformations within the Precambrian formations indicate its antiquity, while the continuity of Kaddam lineament over DVP suggests its Tertiary reactivation. The morpho-tectonic response of the Godavari and Kaddam rivers in this area depict southward tilt of the fault block west of Kaddam fault during Quaternary. In the given set-up we postulate a greater role of crustal loading of the Deccan traps, and its rapid erosional unloading during Late Cenozoic intensified monsoon conditions as one of the causative factors for the above neotectonic response demanding further detailed work on the KLF and elsewhere in the peripheral regions of DVP encountered by active faults and old fractures.
机译:在德肯火山省(DVP)东部边缘以及印度安得拉邦阿迪拉巴德和卡里姆纳加尔地区前寒武纪地形中进行的基于实地和图像的研究显示,戈达瓦里河和卡丹河对卡丹线粒体断裂的强烈反应(KLF)系统。前寒武纪地层中的脆性到韧性变形表明它是古代,而Kaddam谱系在DVP上的连续性表明其第三系复活。该地区的戈达瓦里河和卡达姆河的地貌构造响应反映了第四纪期间卡达姆断裂以西的断层块向南倾斜。在给定的构造中,我们假定Deccan圈闭的地壳加载及其在晚新生代加剧季风条件下的快速侵蚀性卸载具有更大的作用,这是上述新构造响应的原因之一,需要在KLF和其他地方进行进一步的详细研究在活动断裂和旧裂缝中遇到的DVP外围区域。

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