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Characteristics and evolution of strike-slip tectonics of the Liaohe Western Sag,Bohai Bay Basin

机译:渤海湾盆地辽河西部凹陷走滑构造特征与演化

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摘要

Because of its rich oil and gas resources and the special tectonic location of the Liaohe Western Sag(the Tanlu Fault traverses the sag),Bohai Bay Basin,a detailed study of its strike-slip tectonics is significant in revealing the sag's tectonic evolution,its control on hydrocarbon accumulation,and the activity history of the northern section of the Tanlu Fault in the Cenozoic.Through systematic structure analysis of 3D seismic data of the Liaohe Western Sag,combined with balanced section analysis,a variety of structural features in relation to right-lateral strike-slip faults,such as echelon normal faults, "comb"structure," flower"structure, "interpretable" and "buried" strike-slip faults have been revealed exist in the Liaohe Western Sag.According to the research in this paper,the complex structural phenomena in the Liaohe Western Sag could be reasonably interpreted as right-lateral strike-slip activity and the strikeo-slip activities of the Liaohe Western Sag began in the early Oligocene.The activity was weak at the beginning(E3S1-2),then strengthened gradually and reached its strongest level in the late Oligocene(E3dl).In the Miocene,the strike-slip activity was low and then strengthened significantly once again from the Pliocene to the present.It is speculated that the entire northern section of the Tanlu Fault has had a similar evolution history since the Oligocene.
机译:由于其石油和天然气资源丰富,辽河西部凹陷的特殊构造位置(Tanlu断层遍历凹凸),渤海湾盆地,对其防滑构造的详细研究在揭示了落下的构造演变方面具有重要意义,其对乳房坦鲁故障北部北部的活性历史的控制。用辽河西部凹陷3D地震数据的系统结构分析,结合平衡段分析,各种结构特征与右侧 - 辽西西部落下的辽西西部落下时,辽西西部落下的梯队正常断层(如梯队),“梳理”结构,“埋藏”和“埋藏”的防滑断层存在。纸质,辽河西部凹陷中的复杂结构现象可以合理地解释为右侧防滑活动,辽河西部落下的三次汗水活动开始于早期的olig ocene。开始于开始(E3S1-2)的活性较弱,然后逐渐加强并达到其晚期寡核苷(E3DL)中最强的水平。在中间烯中,脱局活性低,然后再次加强概括了本质。据推测,坦尔故障的整个北部部分以来寡核苷酸以来具有类似的演化历史。

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