渤海海域走滑断裂叠合特征与成因机制
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摘要
以全三维地震构造解释为基础,结合构造物理模拟、构造样式解析和磷灰石裂变径迹分析等研究,探讨渤海海域新生代走滑断裂的构造特征与成因机制。研究结果表明,渤海海域新生代郯庐走滑断裂在古近系沙河街组四段沉积末期完成了从左旋走滑到右旋走滑的转变,总体经历3期明显走滑活动。渤海海域走滑断裂具有多期次、多性质应力叠合的特征,根据不同强度、不同性质、不同配比条件下的叠合方式,可划分为伸展-走滑叠合、伸展-挤压叠合、挤压-走滑叠合3大成因类型和15种典型构造样式。受新生代太平洋板块俯冲方向和速率多次变化的影响,渤海海域地壳薄化伸展和走滑拉分作用并存,但在不同时期和地区,两者叠合配比差异明显,导致断裂体系的差异叠合性和凹陷结构的分区性。依据断裂叠合特征,渤海海域可以划分为辽西S型弱走滑区、辽东辫状强走滑区、渤西共轭中等走滑区、渤东帚状中等走滑区和渤南平行强走滑区5大叠合构造区,不同叠合构造区油气差异富集特征不同。
Based on the 3 D seismic structure interpretation of Bohai Sea, combined with physical modeling of structure, structural style analysis and apatite fission track simulation, the structural characteristics and genetic mechanism of the Cenozoic strike-slip faults in Bohai Sea were investigated. The results show that Tanlu strike-slip fault experienced three stages of strike-slip activities in the Cenozoic,and the transition from left-lateral strike to right-lateral strike-slip was completed at the end of the fourth member of the Shahejie Formation. The strike-slip faults in the Bohai Sea have the characteristics of multi-stage and multi-strength stress superposition.According to the superimposed forms of different strengths, different properties and different ratios, they can be divided into three major genetic types, stretch-slip superimposed, stretch-extrusion superimposed and extrusion-slip superimposed, and fifteen typical structure patterns. Affected by multiple changes in the direction and rate of subduction of the Cenozoic Pacific plate, the difference between the Cenozoic extension and the strike-slip in the Bohai Sea area leads to the diversity of the fault system and the zoning of the depression structure. According to superimposition features of faults, the Bohai Sea area can be divided into the Liaoxi S-type weak strike-slip zone,Liaodong braided strong strike-slip zone, Boxi conjugated medium strike-slip zone, Bodong brush structure medium strike-slip zone and Bonan parallel strong strike-slip zone. These zones differ in oil and gas accumulation features.
Based on the 3 D seismic structure interpretation of Bohai Sea, combined with physical modeling of structure, structural style analysis and apatite fission track simulation, the structural characteristics and genetic mechanism of the Cenozoic strike-slip faults in Bohai Sea were investigated. The results show that Tanlu strike-slip fault experienced three stages of strike-slip activities in the Cenozoic,and the transition from left-lateral strike to right-lateral strike-slip was completed at the end of the fourth member of the Shahejie Formation. The strike-slip faults in the Bohai Sea have the characteristics of multi-stage and multi-strength stress superposition.According to the superimposed forms of different strengths, different properties and different ratios, they can be divided into three major genetic types, stretch-slip superimposed, stretch-extrusion superimposed and extrusion-slip superimposed, and fifteen typical structure patterns. Affected by multiple changes in the direction and rate of subduction of the Cenozoic Pacific plate, the difference between the Cenozoic extension and the strike-slip in the Bohai Sea area leads to the diversity of the fault system and the zoning of the depression structure. According to superimposition features of faults, the Bohai Sea area can be divided into the Liaoxi S-type weak strike-slip zone,Liaodong braided strong strike-slip zone, Boxi conjugated medium strike-slip zone, Bodong brush structure medium strike-slip zone and Bonan parallel strong strike-slip zone. These zones differ in oil and gas accumulation features.
引文
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[9]索艳慧,李三忠,刘鑫,等.中国东部NWW向活动断裂带构造特征:以张家口-蓬莱断裂带为例[J].岩石学报,2013,29(3):953-966.SUO Yanhui,LI Sanzhong,LIU Xin,et al.Structural characteristics of NWW-trending active fault zones in East China:A case study of the Zhangjiakou-Penglai fault zone[J].Acta Petrologica Sinica,2013,29(3):953-966.
[10]龚再升,蔡东升,张功成.郯庐断裂对渤海海域东部油气成藏的控制作用[J].石油学报,2007,28(4):1-10.GONG Zaisheng,CAI Dongsheng,ZHANG Gongcheng,et al.Dominating action of Tanlu Fault on hydrocarbon accumulation in eastern Bohai Sea area[J].Acta Petrolei Sinica,2007,28(4):1-10.
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[16]李德生.渤海湾含油气盆地的地质和构造特征[J].石油学报,1980,1(1):7-20.LI Desheng.Geology and structural characteristics of Bohai Bay,China[J].Acta Petrolei Sinica,1980,1(1):7-20.
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[18]刘和甫,梁慧社,李晓清,等.中国东部中新生代裂陷盆地与伸展山岭耦合机制[J].地学前缘,2000,7(4):477-486.LIU Hefu,LIANG Huishe,LI Xiaoqing,et al.The coupling mechanisms of Mesozoic-Cenozoic rift basins and extensional mountain system in eastern China[J].Earth Science Frontiers,2000,7(4):477-486.
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