论亚洲东部的陆缘型壳体  

ON THE CONTINENTAL MARGIN REGION TYPE CRUSTOBODIES IN EASTERN ASIA

作　　者：陈国达[1] 

机构地区：[1]中南工业大学地洼学说成矿学研究所

出　　处：《中南工业大学学报》1999年第4期331-335,共5页Journal of Central South University of Technology(Natural Science)

基　　金：国家自然科学基金;国家教育部博士点基金

摘　　要：在东亚大陆的东缘有３个陆缘型壳体，分别称为东北亚、东亚及东南亚陆缘壳体．它们并非有些学者所认为的属于过渡型壳体，而实际是已演化达到高级成熟度的大陆型壳体，只是由于它们在形成以后，因受东亚陆缘扩张运动的改造，以致被拉断伸展而厚度减薄，遂造成了似乎是过渡型地壳的假象．这些陆缘壳体已演化到地洼阶段，其中既有继承自历代前身的前地槽型、地槽型及地台型矿床，又产生了自身的地洼型矿产．There are three continental margin region type crustobodies in the east margin of the continent of East Asia, called the Northeast, the East, and the Southeast Asia continental margin crustobodies. They are not transitional crustobodies as some scholars considered, but continental crust type crustobodies, which have evolved into a high level stage diwa stage. They take a false appearance of the transitional crustobodies, as their crust has been thinned by splitting and extension due to continental margin spreading of East Asia since they formed. Inside them, there are pregeosyncline type, geosyncline type, and platform type deposits inherited from every predecessors, as well as diwa type deposits themselves.

关 键 词：陆缘壳体 陆缘扩张 东亚 亚洲 

分 类 号：P736.15[天文地球—海洋地质] P541[天文地球—海洋科学]