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Characteristics of 2004 tsunami deposits of the northern Tamil Nadu coast, southeastern India

机译:印度东南部泰米尔纳德邦北部海岸2004年海啸沉积物的特征

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The 2004 Indian Ocean tsunami left significant sand deposits along the coastal tract of southeast India (Tamil Nadu state). These deposits serve as a benchmark to understand the effects of present day tsunami on the coastline. Additionally, the geological signatures of tsunami in the coastal stratigraphy can assist in providing modern analogs for identification and interpretation of ancient tsunami. This article presents the field observations of tsunami deposits, their internal stratigraphy and foraminiferal distribution, all of which varied from north to south depending upon coastal geomorphology, near shore bathymetry and sediment sources. In a few places, the tsunami deposits have been reworked due to subsequent events that caused modification in the internal stratigraphy. The tsunami deposits of the northern Tamil Nadu coast comprise at least 50% or more reworked foraminiferal specimens, indicating that the tsunami sediments may have been derived from a paleostrandline from a water depth of at least 45 m.
机译:2004年印度洋海啸在印度东南部沿海地区(泰米尔纳德邦)留下大量砂土沉积物。这些沉积物可作为了解当今海啸对海岸线影响的基准。此外,沿海地层中海啸的地质特征可以帮助提供现代类似物,以识别和解释古代海啸。本文介绍了海啸沉积物,其内部地层学和有孔虫分布的野外观测,所有这些都根据沿海地貌,近岸测深法和沉积物来源从北向南变化。在某些地方,由于随后发生的事件导致内部地层发生了变化,海啸沉积物已被重新处理。泰米尔纳德邦北部海岸的海啸沉积物包含至少50%或更多的经过改造的有孔虫标本,这表明海啸沉积物可能是从至少45 m水深的古兰经中提取的。

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