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青藏高原隆起与东海陆架抬升的对比研究
引用本文:赵松龄,于洪军.青藏高原隆起与东海陆架抬升的对比研究[J].海洋科学,1996,20(3):56-62.
作者姓名:赵松龄  于洪军
作者单位:中国科学院海洋研究所!青岛266071
基金项目:国家自然科学基金!编号49291100
摘    要:青藏高原的强烈隆起始于第四纪初期,目前仍处于强烈隆起阶段。根据钻孔和浅地层剖面仪测量等大量资料的研究,更新世以来东海陆架的周边也处于快速隆起时期,冰期海退时期的地壳回弹作用有可能加大了东海陆架区的地壳上升量。

关 键 词:青藏高原  东海  陆架  抬升  第三纪  砂岩
收稿时间:3/5/1996 12:00:00 AM

STUDY ON COMPARISON THE UPLIFT OF THE TIBETAN PLATEAU WITH RISE OF THE EAST CHINA SEA SHELF
Zhao Songling and Yu Hongjun.STUDY ON COMPARISON THE UPLIFT OF THE TIBETAN PLATEAU WITH RISE OF THE EAST CHINA SEA SHELF[J].Marine Sciences,1996,20(3):56-62.
Authors:Zhao Songling and Yu Hongjun
Abstract:The stronger uplift of the Tibetan Plateau began in early Quaternary and it's going on now. Based on the study of many cores data and shallow layer profiler records, all around the East China Sea shelf were also in rapid rising period since Pleistocene. During low-sealevel stage in glacial periods, the rebound maybe increase the ascendind measurement in the East China Sea. During the upper stage of Late Pleistocene, the desertization occurred in the East China Sea shelf. The large range of Tertiary sandstone was the most important material source. The Changjiang River and Yellow River didn't reach the shelf region during low -sealevel stage in glacial periods.
Keywords:Tibetan Plateau  East China Sea shelf  Uplift  Tertiary sandstone
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