Baseline geophysical data for hazard management in coastal areas in relation to earthquakes and tsunamis

K. Murthy
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引用次数: 1

Abstract

A systematic study of geophysical data of the Eastern Continental Margin of India was taken up to identify the land–ocean tectonic lineaments over the east coast of India and the possible neotectonic activity associated with them. These studies helped in delineating the offshore extension of some of the coastal lineaments. Analysis of magnetic, gravity and shallow seismic data, combined with reported seismicity data, indicates moderate seismicity associated with some of these land–ocean tectonics of the Eastern Continental Margin of India. The coastal/offshore regions of Vizianagaram (north of Visakhapatnam) and Ongole of the Andhra Pradesh margin and the Puducherry shelf of the Tamil Nadu margin have been identified as zones of weakness where neotectonic activity has been established. Bathymetry data over the Eastern Continental Margin of India revealed the morphology of the shelf and slope of this margin, which in turn can be used as the baseline data for tsunami surge models. Detailed bathymetry map and sections of the Nagapattinam–Cuddalore shelf (from 10.5° to about 12°N) indicate that one of the main reasons for the higher run-up heights and inundation in the Nagapattinam–Cuddalore coast during the Indian Ocean Tsunami of 26 December 2004 could be the concave shape of the shelf with a gentle slope, which might have accelerated the tsunami surge to flush through at a rapid force. Structural control also appears to be a contributing factor for the tsunami surge.
用于沿海地区地震和海啸灾害管理的基线地球物理数据
本文对印度东部大陆边缘的地球物理资料进行了系统的研究,以确定印度东海岸的陆海构造线及其可能的新构造活动。这些研究有助于划定一些沿海地貌的离岸延伸。对磁、重、浅层地震资料的分析,结合已报道的地震活动性资料,表明印度东部大陆边缘的一些陆-海构造与中等地震活动性有关。Vizianagaram(维萨卡帕特南北部)和安得拉邦边缘的Ongole以及泰米尔纳德邦边缘的Puducherry陆架的沿海/近海区域已被确定为新构造活动建立的薄弱带。印度东部大陆边缘的测深数据揭示了该边缘的陆架和斜坡的形态,这反过来又可以作为海啸潮模型的基线数据。Nagapattinam-Cuddalore大陆架的详细测深图和剖面(从10.5°到约12°N)表明,2004年12月26日印度洋海啸期间,Nagapattinam-Cuddalore海岸上升高度和淹没程度较高的主要原因之一可能是大陆架的凹形和缓坡,这可能加速了海啸浪潮以快速的力量冲过。结构控制似乎也是海啸激增的一个促成因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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