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首页> 外文期刊>Journal of the Geological Society of India >Late holocene storm records from lower reaches of Narmada valley, Western India
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Late holocene storm records from lower reaches of Narmada valley, Western India

机译:印度西部纳尔默达河谷下游的全新世风暴记录

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摘要

Storms from the Arabian Sea are the most significant meteorological feature in western India that brings extreme rainy days together with catastrophic flooding. The present study reports two such palaeo-storm horizons at 1.16 m and 3.2 m above the present day water level in the Narmada channel, 56 km inland based on sedimentology and foraminiferal records. Both the horizons show similar sediment facies and foraminiferal assemblage. The present findings instigate to look for such new sites and build palaeo-storm records for western India.
机译:来自阿拉伯海的风暴是印度西部最重要的气象特征,使极端的雨天和灾难性的洪水泛滥。根据沉积学和有孔虫记录,本研究报告了纳尔默达河通道内陆56 km的两个水平面,分别高于现今水位1.16 m和3.2 m。两种层位都显示出相似的沉积相和有孔虫组合。目前的发现促使人们寻找这样的新地点,并为印度西部建立古风暴记录。

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