黄骅盆地孔西构造带的构造几何学特征

英文篇名：Tectonic Geometric Characters of Kongxi Structural Belt
中文刊名：北京大学学报(自然科学版)
英文刊名：Acta Scicentiarum Naturalum Universitis Pekinesis
作者：张俊 ; 潘懋 ; 漆家福 ; 杨攀新
英文作者：ZHANG Jun 1) \ PAN Mao 1) \ QI Jiafu 2) \ YANG Panxin 1) ( 1) School of the Earth and Space Science ; Peking University ; Beijing ; 100871 ; 2) Department of Geology ; University of Petroleum ; Beijing ; 102200)
中文关键词：构造样式 ; 逆冲构造 ; 孔西构造带
英文关键词：the structural style ; thrust ; Kongxi structural belt
出版日期：2002-07-20
机构：北京大学地球与空间科学学院,北京大学地球与空间科学学院,石油大学地科系,北京大学地球与空间科学学院北京,100871 ,北京,100871 ,北京,100021 ,北京,100871
年：2002
期：04
出版单位：北京大学学报(自然科学版)

摘要

地震和钻井资料揭露的孔西构造带前第三系潜山的地质特征可以归纳为 :构造带总体上不对称 ;构造带内部有地层重复现象 ;石炭—二叠系地层的位置明显高于两侧的同一地层的高度。用由 3～ 4条向东倾斜的逆冲断层组成的叠瓦扇构造模式能够比较合理地解释上述地质特征。该带向东倾斜的逆冲叠瓦状断层组主要影响前侏罗系地层 ,侏罗—白垩系与卷入逆冲构造变形的古生界地层之间有明显的角度不整合。但是部分地段的逆冲断层前锋也已切割到侏罗—白垩系底部 ,表明在侏罗—白垩系发育初期仍有逆冲作用。沿着潜山构造带走向 ,逆冲构造样式有所变化。
Kongxi buried hill shows following features in the seismic profiles:the structures are asymmetric.There is flexural syncline on the east side and a monocline on the west side.Asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle.The Permo\|Carboniferous system of both sides almost lie in the same slope and the events of Cambrian or upper Proterozoic are continuous from east to west.The phenomenas suggest that Kongxi buried hill could be a thrust belt been traced which consists of reverse faults.The imbricate faults mainly effect Pre\|Jurassic strata.There are obvious angular unconformity between Jurassic\|Cretaceous system and Paleozoic involved deformation of thrust.The thrust front in some place has cut off the beds of Jurassic\|Cretaceous system.The structural style of the thrust structure changes along the strike of the Kongxi buried hill.

引文

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