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Holocene morphological modification of South West coast of India: Evidence from the palaeo-deposits of Meenachil river basin, Kerala

机译:印度西南海岸的全新世形态改造:来自喀拉拉邦Meenachil流域古沉积的证据

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摘要

Kerala State of Indian sub-continent unfortunately possesses a highly imperfect geological record compared to other states. The occurrence of Tertiary and Recent deposits as longitudinal outcrops paralleling the Western coast has led to the view thatKerala was under the influence of local marine environments to a minor extent in the geological past. The present study has created an insight into the morphological modification of the south western coast of India by depicting the textural characteristics of the palaeo-deposits of Meenachil River Basin. The existing course of the Meenachil River, its two tributaries - Pannagan Thodu and Meenadom Ar and the flood plains of the same were also investigated for textural analysis and the textural dispersionmodel was evolved using Arc GIS (8.3version) to find out the influenced geomor-phological configuration of the area. 14C dating of the palaeodeposits was also done to evolve the chronology of deposition. It is suggested that the occurrence of palaeo-deposits of sand in the Meenachil river basin had their origin in consequent to the Holocene eustatic sea level fluctuations and tectonism.
机译:与其他州相比,印度次大陆的喀拉拉邦拥有非常不完善的地质记录。第三纪和新近沉积物的出现是与西海岸平行的纵向露头,这导致喀拉拉邦在过去的地质环境中受到当地海洋环境的影响程度较小。本研究通过描绘Meenachil流域的古沉积物的纹理特征,从而对印度西南海岸的形态变化有了深刻的认识。还研究了Meenachil河及其两条支流Pannagan Thodu和Meenadom Ar的现有河道以及该河的洪泛平原进行纹理分析,并使用Arc GIS(8.3版本)对纹理扩散模型进行了演化,以找出受影响的地质-该区域的形态配置。还对古沉积物进行了14 C测年,以发展沉积的时间顺序。有人认为,Meenachil流域的古沉积物砂的发生是由于全新世的海平面波动和构造运动引起的。

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