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《Chinese Geology》 2003-02
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Several problems about the Paleoproterozoic geology of eastern Liaodong

CHENRong-du,LIXian-dong,ZHANGFu-sheng(LiaoningInstituteofGeologicalExploration,Dalian116100,Liaoning,China)  
The results of new regional survey has validated the sequence of the Paleo proterozoic Liaohe Group es-tablished in eastern Liaoning in the1970s and the existence of the N-S facie s change in the Liaohe Group.The Liaohe Group has all crossed the Yalu River and is distributed over various parts of the Langlin massif.Most of the Langlin Gro up is equivalent to the Liaohe Group.The main part of the original sedimentary b asin of the Liaohe Group occurs as an E-W-trending narrow stripe.It takes the Ar chean continental crust as the base;in the basin bimodal volcanic rocks are deve loped.The tectonic attribute is the continental rift.In a few individual cen-tral parts,there appears oceanic crust separated from the massif.The paper a lso discusses the cause for the differ-ence in geology between the northern and southern Archean continental blocks of the ancient basin.
【CateGory Index】: P534.3
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