The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
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