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青藏高原湖泊涨缩的新构造运动意义
引用本文:陈兆恩,林秋雁.青藏高原湖泊涨缩的新构造运动意义[J].地震,1993(1):29-40,52.
作者姓名:陈兆恩  林秋雁
作者单位:国家地震局分析预报中心 (陈兆恩),中国科技大学研究生院(林秋雁)
摘    要:青藏高原位于我国的西南部,平均海拔4000—5000m。第四纪以来强烈的新构造运动,引起地壳大幅度的隆起,迫使湖泊出现了大规模的退缩及迁移。新的湖泊不断产生或扩大,古老的湖泊又不断消亡或缩小,形成了湖泊变化与构造活动周期的对应性。本文在分析了青藏高原的地貌、第四纪地质,特别是活断层及地震活动性研究的基础上,对于高原≥4km~2的367个湖泊进行了卫片解译,并取得了较好的效果。

关 键 词:地震活动性  湖泊  涨缩  新构造运动

SIGNIFICANCE OF NEOTECTONIC MOVEMENT OF LAKE EXTENSION AND SHRINKAGE IN QINGHAI-TIBET PLATEAU
Chen Zhaoen Lin Qinyan.SIGNIFICANCE OF NEOTECTONIC MOVEMENT OF LAKE EXTENSION AND SHRINKAGE IN QINGHAI-TIBET PLATEAU[J].Earthquake,1993(1):29-40,52.
Authors:Chen Zhaoen Lin Qinyan
Abstract:Qinghai-Tibet plateau is located in Southwest China with average elevation of 4000-5000 m. Since Quaternary strong neotectonic movement has caused large crustal uplifting, resulted in large-scale lake shrinking and migration. New lakes contineously formed and old lakes were disappeared or shrinked. There was a periodic relation between lake change and neotectonic activity. Based on analyses of geomorpr-ology, Quaternary geology, especially active faults and seismicity, this paper proposed the interpretation of satellite images of 367 lakes (>4Km2 in area) and a quite good result was obtained.
Keywords:lake geometry  lake migration
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