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tai hu de xing cheng he yan bian guo cheng
Author(s): Hong Xueqing
Pages: 87-
99
Year: 1991
Issue:
4
Journal: Marine Geology & Quaternary Geology
Keyword: 太湖; 全新世; 成因; 演变;
Abstract: 本文从沉积学、地层学、地貌学、考古学和历史地理学角度,综合分析了太湖的成因和演变。认为地壳沉降与海面上升是构成江南碟形洼地的内外动力,为太湖的形成奠定了基础。全新世海侵最盛时,太湖海湾水深潮急、泻湖、滨海沼泽围绕海湾分布。随南部湾口沙嘴封堵,海湾趋于消失,陆地扩大,遗址增多。3700a来,海面回升,湖面逐渐扩展,形成现代太湖。
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