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Re-determining source faults of the Upper Cretaceous Putaohua oil layer in Sanzhao sag of Songliao Basin, NE China

机译:内蒙古松辽盆地三肇凹陷上白垩统葡萄花油层源断层的重新确定

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From the deformation characteristics of two walls of a fault caused by fault activities, the activation of faults in the critical moment of oil and gas accumulation (structural inversion period) was analyzed to determine the source faults in the Upper Cretaceous Putaohua oil layer of the Sanzhao sag in Songliao Basin. Based on the previous classification and research results of activity patterns of the faults in the Sanzhao sag, the analysis of the structural deformation characteristics during the deposition of the 2nd and 3rd members of the Upper Cretaceous Nenjiang Formation and the inversion reveals that the feature of cutting to T06 reflection layer (bottom interface of the third member of the Nenjiang Formation) can not be taken as the basis to judge whether the faults were activated during the inversion or not. But during the structural inversion period, the structural deformation caused by faults would lead to fault-propagation inverted folds and fault-bend inverted folds, which would further lead to obvious deformation differences between hanging walls and foot walls of faults, this can be taken as the basis to determine if the faults were activated or not in the inversion period, and then the source faults of the Putaohua oil layer can be determined. Furthermore the source faults can be divided into two kinds, concealed faults and penetrating faults, according to if the source faults cut through layers of inversion period or not. These two kinds of source faults show more obvious control over the planar oil distribution in the Putaohua layer than the previous study results.
机译:从断层活动引起的断层两壁变形特征出发,分析了油气成藏关键时刻的断层活动(构造反转期),确定了三肇上白垩统葡萄花油层的源断层。松辽盆地下陷。根据先前的分类和三肇凹陷断层活动模式的研究结果,对上白垩统嫩江组二,三段沉积和反演过程中的构造变形特征进行了分析,揭示了cutting陷特征。以T06反射层(嫩江组第三段底部界面)为基础,不能判断断层是否在反转过程中被激活。但在构造反转期间,断层引起的结构变形会导致断层传播倒转褶皱和断层弯曲倒转褶皱,进而导致断层的悬壁和脚底壁之间存在明显的变形差异。以此为基础确定断层是否在反转期内被激活,进而确定葡萄花油层的源断层。此外,根据源断层是否穿过反转周期层,将源断层分为隐性断层和穿透性断层两种。与以前的研究结果相比,这两种源断层显示出对葡萄花层中平面油分布的明显控制。

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