首页> 外文期刊>Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences >Geomorphic expression of late Quaternary sea level changes along the southern Saurashtra coast, western India
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Geomorphic expression of late Quaternary sea level changes along the southern Saurashtra coast, western India

机译:印度西部索拉什特拉南部海岸第四纪晚期海平面变化的地貌表达

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摘要

Geomorphic expression of land-sea interaction is preserved in the form of abandoned cliffs, marine terraces, shore platforms and marine notches along the southern Saurashtra coast. These features have been used to ascertain the magnitude of sea level changes during late Quaternary. Notch morphology and associated biological encrustation have been used to estimate the magnitude and duration of palaeo-sea strands. Marine notches and other erosive features occurring between 12 and 15 m above the present Biological Mean Sea Level (BMSL) are attributed to the last interglacial corresponding to the Marine Isotopic Stage 5 (MIS-5). However, 6 to 9 m upliftment of the coastal fringe is attributed to this sea level. The second major high sea strand was identified during the mid-Holocene when the sea rose 2 m above the present level. Notches corresponding to this high sea level are recorded 4 to 5 m above the present BMSL.
机译:陆海相互作用的地貌表现形式是沿南部索拉什特拉海岸沿岸的废弃悬崖,海洋阶地,海岸平台和海洋凹口形式保存的。这些特征已被用来确定第四纪晚期海平面变化的幅度。缺口形态和相关的生物结壳已被用来估计古海链的大小和持续时间。在当前生物平均海平面(BMSL)之上12至15 m之间发生的海洋刻痕和其他侵蚀特征归因于与海洋同位素第5阶段(MIS-5)相对应的最后一个冰间期。但是,沿海边缘隆起6至9 m是由于该海平面。在全新世中期发现了第二条主要的高海带,当时海平面上升了2 m以上。在当前BMSL上方4至5 m处记录了与该高海平面相对应的凹口。

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