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首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Late Quaternary drainage disorganization, and migration and extinction ofthe Vedic Saraswati [Review]
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Late Quaternary drainage disorganization, and migration and extinction ofthe Vedic Saraswati [Review]

机译：韦达奇·萨拉斯瓦蒂（Vedic Saraswati）的第四纪晚期排水系统混乱，迁移和灭绝[评论]

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摘要

Several lines of geological evidence confirm the existence of a high-energy fluvial regime in western Rajasthan during the Late Quaternary period. Geomorphic description of the extinct river system matches well with the Saraswati River described so vividly in the Rig Veda. The Vedic river which presumably flowed parallel to the Aravalli Mountains during its initial stages, migrated westward during neotectonic. uplift of the Aravalli Mountains. The neotectonic movements, which brought about the down-sagging of the northern part of Aravalli Mountains also forced the Yamuna River to swap its original course to flow across the flattened 'mountain'. The river presumably pirated the Saraswati waters while it drifted eastward to join the Ganges.
机译：几条地质证据证实，第四纪晚期，拉贾斯坦邦西部存在着高能河流系统。灭绝河系的地貌描述与“索格维达”中生动描述的萨拉斯瓦蒂河非常吻合。吠陀河初期大概平行于阿拉瓦利山脉，在新构造时期向西迁移。阿瓦瓦利山脉的隆起。新构造运动导致了阿拉瓦利山脉北部的下陷，也迫使亚穆纳河改变了原来的路线，流经平坦的“山脉”。这条河在向东漂移以加入恒河的同时，可能在萨拉斯瓦蒂河上造成了海盗。

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