Textural Characteristics and Depositional Environment of a Late Quaternary Alluvial Plain of Haryana

Tarasha Chitkara, O. Thakur, Anupam Sharma
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Abstract

The present study deals with the textural characteristics of the sediments from the exposed palaeochannel situated at Dhyangla village near Ladwa, district of Kurukshetra in north-western Haryana. It is a part of vast alluvial plains of India. Samples were taken from a 3 m thick exposed section. Grain size distribution and Palynofacies analyses of these sediments were carried out to study their textural parameters and the organic matter content respec-tively. Sediments are mostly fine to medium grained sand with silt percentage increasing upwards in the section. These sediments are mostly unimodal showing the grain size population controlled by a single type of grain size, mostly sand. Further the sand samples are moderately well sorted and mesokurtic in nature. Samples with silt are poorly sorted and leptokurtic with positive skewness, denoting those sediments have already sorted elsewhere in the high energy environment and are now transported and modified by the low energy environment. Palynofacies analysis also shows the presence of amorphous particles in the silt samples which indicate low energy environment of the sequence while presence of black debris in the sand samples indicates high energy depositions environment.
哈里亚纳邦晚第四纪冲积平原的结构特征与沉积环境
本文研究了哈里亚纳邦西北部Kurukshetra地区Ladwa附近Dhyangla村裸露古河道沉积物的结构特征。它是印度广阔的冲积平原的一部分。样品取自3米厚的暴露切片。对这些沉积物进行粒度分布和孢粉相分析,分别研究其结构参数和有机质含量。沉积物以细粒至中粒砂为主,含沙量呈上升趋势。这些沉积物大多是单峰的,显示了由单一类型的粒度控制的粒度种群,主要是沙子。此外,砂样分选较好,属中粒质。含粉土的样品分选差,呈细峰状,偏度为正,表明这些沉积物在高能环境中已经被其他地方分选,现在被低能环境输送和修饰。孢粉相分析还表明,粉质样品中存在无定形颗粒,表明层序的低能量环境,而砂质样品中存在黑色碎屑,表明层序的高能量沉积环境。
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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