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胶南隆起北缘中段左行正滑韧性剪切带研究

A STUDY OF THE LEFT-LATERAL NORMAL SLIP DUCTILE SHEAR ZONE IN THE NORTH MARGIN OF JIAONAN UPLIFT

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【作者】 张长厚顾德林宋鸿林吴正文陈建强朱忠安郁宏任有保

【Author】 Zhang Changhou Gu Delin Song HonglinWu Zhengwen Chen Jianqiang(China University of Geosciences,Beijng )Zhu Zhong An Yuhong Ren Youbao(Gan=hou Geological School, Jiangxi Province) (Regional Geological Survey Brigade, Shandong Province)

【机构】 中国地质大学赣州地质学校山东省区域地质调查队山东省区域地质调查队 北京北京北京

【摘要】 在详细的野外地质填图的基础上,通过各种尺度的构造研究和系统的应变测量,确定了胶南隆起北缘中段的大型左行正滑韧性剪切带的存在及其延展范围,并提出了确定韧性剪切带边界的构造几何学准则。研究了该韧性剪切带的几何学和运动学特征及变形机制,估算了其剪切位移量(大于7557m)及形成时的差异应力(σ13=94.6~114.4MPa)。该韧性剪切带可以作为胶南隆起的北部边界,但不是重要的板块碰撞边界。

【Abstract】 Based on the detailed field regional geological mapping and research of microscopicstructures, as well as systernatic strain measurement of deformed mineral, a large-scaleleft-lateral normal slip ductile shear zone in the north margin of Jiaonan uplift is delimited.The structural geometric criterion is provided to ascertain the edge of the ductile shearzone. The geometric. kinematic features and deformation mechanism of the ductile shearzone are clarified. and the estimate for the displacement of the ductile shear zone (morethan 7 557 m) and the volume of the paleo-differential stress (94. 6~ 114. 4 MPa) aremade. It is reasonable to infer that the left-lateral normal slip ductile shear zone extendingalong the margin of the Jiaonan uplift is not an important plate collision zone.

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