长春市新构造运动特征
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摘要
本文主要叙述了研究区内的活动性断裂,第四纪以来形成的褶皱构造,第四纪隆起和拗陷,地震活动,火山活动,河流的迁移,冰期及沉积物,新构造期的地壳运动。长春市新构造运动特征同其他地区一样,具有新构造运动的普遍性、多样性、继承性、不均衡性及间歇性等。
This paper mainly describes the research in the active faults in the study area,fold structures since the formation of the Quaternary,Quaternary salient and trough,seismic activities,volcanic activities migration of river,ice age and sediments,the earth's crust movement.Changchun new tectonic movement characteristics are similar to other regions,have some characteristics in neotectonic intermittence,differention of neotectonics,neotectonic generality,neotectonic inheritance,etc.
This paper mainly describes the research in the active faults in the study area,fold structures since the formation of the Quaternary,Quaternary salient and trough,seismic activities,volcanic activities migration of river,ice age and sediments,the earth's crust movement.Changchun new tectonic movement characteristics are similar to other regions,have some characteristics in neotectonic intermittence,differention of neotectonics,neotectonic generality,neotectonic inheritance,etc.
引文
[1]李军敏.长春—四平地质新构造运动[D].吉林:吉林大学,2004.
[2]吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1988.
[2]吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1988.
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