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Factors guiding tsunami surge at the Nagapattinam-Cuddalore shelf,Tamil Nadu, east coast of India

机译:印度东海岸泰米尔纳德邦Nagapattinam-Cuddalore架子海啸激增的因素

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摘要

The Tamil Nadu (India) margin, in particular the Nagapattinam-Cuddalore shelf was the worst affected by the tsunami surge and inundation caused by the great Sumatra earthquake of 26 December 2004 (M sub(w) 9.3). Surge heights in this part were of the order of 2 to 5 m, with inundation of the order of few hundred metres into the interior coast, thus causing huge loss of human life and property. Several reasons were attributed to the unusual surge in this part of the Tamil Nadu margin, the main reason being its relative proximity to the origin of the event, apart from the concave nature of the shelf with a gentle gradient. A detailed analysis of geophysical data of the Nagapattinam-Cuddalore shelf is presented. The results indicate that the structure of the underlying basement, the morphology and the land-ocean tectonics are the main guiding factors for the run-up heights in case of the Nagapattinam-Cuddalore shelf. The faultcontrolled basement structure, and a straight coastline with narrow and gentle shelf have helped in rapid transgression of the surge inundating the coastal area.
机译:泰米尔纳德邦(印度)边缘,特别是纳加帕蒂纳姆-库达洛尔大陆架,受2004年12月26日苏门答腊大地震引起的海啸激增和洪水泛滥影响最大(M sub(w)9.3)。该部分的浪涌高度约为2至5 m,淹没内陆海岸的高度约为数百米,从而造成巨大的生命和财产损失。泰米尔纳德邦边缘这部分异常隆升的原因有很多,主要原因是它与事件的起因相对接近,除了架子上的凹性和平缓的梯度。介绍了Nagapattinam-Cuddalore架子的地球物理数据的详细分析。结果表明,在Nagapattinam-Cuddalore陆架的情况下,下层基底的结构,形态和陆地-海洋构造是抬升高度的主要指导因素。断层控制的地下室结构,以及平直的海岸线,狭窄而平缓的海岸线,都有助于海浪迅速泛滥,淹没了沿海地区。

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