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地质学报  2004 

泌阳凹陷新生代构造特征与形成机制及其与油气成藏的关系

, PP. 332-344

Keywords: 泌阳凹陷,新生代,构造特征,构造演化

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Abstract:

根据地层层序特征,叠加在东秦岭造山带之上的泌阳凹陷伸展作用可以划分出6个伸展作用幕。核二段沉积前泌阳凹陷以北东―南西向的伸展作用为主,构造变形受以正断层为主兼具左旋走滑分量的唐河―栗园断裂控制。核二段沉积期――廖庄组沉积末期构造应力场发生转变,以北西―南东向伸展作用为主,构造变形主要受以正断层为主兼具右旋走滑分量的泌阳―栗园断裂控制。断裂活动引起上盘构造变形,对先成构造进行改造。廖庄组沉积末期发生区域性的隆升作用,北西―南东向的伸展作用导致边界断裂上盘发生断块掀斜,地层遭受强烈剥蚀。核二段沉积以来尤其是廖庄组沉积末期,受北西―南东向不均匀伸展作用的影响,北西向走滑断层活动并影响盖层构造样式

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