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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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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 identi???ed 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:陆地与海洋相互作用的地貌表现形式是保留下来的悬崖,海洋阶地,海岸平台和南部索拉什特拉海岸沿岸的海槽形式。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被用来估计古海链的幅度和持续时间;海洋缺口和其他侵蚀特征发生在12至15 m之间高于当前生物平均海平面(BMSL)的原因是与海洋同位素第5阶段(MIS-5)相对应的最后一个冰间期。然而,沿海边缘的隆起是由该海平面引起的6至9 m升高。第二个主要的高海线是在全新世中期期间发现的,当时海平面上升了2 m。在当前BMSL上方4至5 m处记录到了高海平面。

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