渤海海域新生代褶皱作用
|
摘要
基于地震资料解释,总结了渤海海域新生代褶皱作用的类型、控制因素及分布。从力学成因上看,渤海海域褶皱作用可以划分为4种类型,即与拉张作用有关的、与扭动作用有关的、与重力滑动诱导的挤压作用有关的和与压实、底辟等重力作用有关的褶皱作用。与拉张和挤压有关的褶皱作用发生在古近纪,分别沿长期活动的控制性断裂和斜坡带分布。与扭动有关的褶皱作用发生在新近纪晚期,主要分布在盆地东部郯庐断裂经过的地方。重力褶皱中的披覆褶皱作用贯穿于整个新生代,分布在凸起上;而盐底辟褶皱作用分布局限,目前仅在盆地南部的莱州湾凹陷有所发现。从目前渤海海域油气勘探实践看,沿断裂带分布的与新近纪晚期扭动褶皱相关的圈闭是有利的储油气构造。
This paper summarizes the types of the Cenozoic folding,their controlling factors and distribution in the Bohai Sea waters based on seismic data interpretations.According to their mechanical genesis,the folding can be classified into four types which are respectively related to extension,wrench,compression induced by gravity sliding,and compaction and diapirism caused by gravity.Extension-related folding and compression-rela-ted folding happened during the Paleogene and these two types of folds are distributed along the long-active main faults and slopes respectively.Wrench-related folding happened during the Neogene and the folds are distributed in the eastern part of the Bohai Bay Basin where the Tanlu fault zone passes by.Among the gravity-related fol-ding types,the drape folding had been active in the whole Cenozoic and the folds are distributed on the salient.While the salt diapirism folding was restricted to certain areas and the faults occur only in the Laizhou Bay sag at the south of the basin.The current exploration results in the Bohai Sea waters show that traps located along the faults and related to the wrench folds of the Late Neogene are favorable for oil and gas accumulation.
This paper summarizes the types of the Cenozoic folding,their controlling factors and distribution in the Bohai Sea waters based on seismic data interpretations.According to their mechanical genesis,the folding can be classified into four types which are respectively related to extension,wrench,compression induced by gravity sliding,and compaction and diapirism caused by gravity.Extension-related folding and compression-rela-ted folding happened during the Paleogene and these two types of folds are distributed along the long-active main faults and slopes respectively.Wrench-related folding happened during the Neogene and the folds are distributed in the eastern part of the Bohai Bay Basin where the Tanlu fault zone passes by.Among the gravity-related fol-ding types,the drape folding had been active in the whole Cenozoic and the folds are distributed on the salient.While the salt diapirism folding was restricted to certain areas and the faults occur only in the Laizhou Bay sag at the south of the basin.The current exploration results in the Bohai Sea waters show that traps located along the faults and related to the wrench folds of the Late Neogene are favorable for oil and gas accumulation.
引文
1李德生.渤海湾含油气盆地的地质构造特征与油气田分布规律[J].海洋地质研究,1981,1(1):11～20
2陆克政,漆家福,戴俊生.渤海湾新生代含油气盆地构造模式[J].北京:地质出版社,1997.251
3汤良杰,万桂梅,周新怀,等.渤海海域新生代构造演化[J].高校地质学报,2008,14(2):191～198
4侯贵廷,钱祥麟,蔡东升.渤海中、新生代盆地构造活动与沉积作用的时空关系[J].石油与天然气地质,2000,21(3):201～206
5Xiao H,Suppe J.Origin of rollover[J].AAPG Bulletin,1992,76:509-529
6葛建党.郯庐断裂在渤中凹陷的构造特征与油气成藏的关系[J].海洋石油,2001,(1):14～20
7刘和甫,李晓清,刘立群,等.伸展构造与裂谷盆地成藏区带[J].石油与天然气地质,2005,26(5):537～552
8漆家福,王德仁,陈书平,等.兰聊断层的几何学、运动学特征对东濮凹陷构造样式的影响[J].石油与天然气地质,2006,27(4):451～459
9邓津辉,周心怀,魏刚,等.郯庐走滑断裂带活动特征与油气成藏关系———以金县地区为例[J].石油与天然气地质,2008,29(1):102～105
10Rowan MG,Kligfield R.Cross section restoration and balancing as aid to seismic interpretion in extensional terranes[J].AAPG Bul-letin,1989,73(8):955-966
11White N J,Jackson J A,MeKenzie D P.The relationship between the geometry of normal faults and that of the sedimentary layers in their hanging walls[J].Journal of Structural Geology,1986,8:897-909
12Gibbs A.Development of extension and mixed-mode sedimentary basins,in continental extensional tectonics[A].In:Coward M P,Dewey J F,Hancock P L,eds.Geological Society Special Publica-tion London,1987,28:19-33
13Williams G,Vann I.The geometry of listric normal faults and de-formation in their hanging-walls[J].Journal of Structural Geology,1987,9:789-795
14Withjack M O,Gallaway S.Active normal faulting beneath a salt layer:an experimental study of deformation patterns in the cover sequence[J].AAPG Bulletin,2000,84(5):627-651
15余一欣,周心怀,汤良杰,等.渤海海域莱州湾凹陷KL112地区盐构造特征[J].地质学报,2008,82(6):731～737
16Lee T Y,Lawver L A.Cenozoic plate reconstruction of southeast Asia[J].Tectonophysics,1995,251:85-138
17Engebretson D C,Cox A,Gordon R G.Relative motions between oceanic and continental plates in the Pacific basin[J].The Geolo-gical Society of America Special Paper206,1985.1-59
18马杏垣,刘和甫,王维襄,等.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,1983,57(1):22～32
19漆家福,张一伟,陆克政,等.渤海湾新生代裂陷盆地的伸展模式及其动力学过程[J].石油实验地质,1995,17(4):316～323
20Maruyama S,Isozaki Y,Kimura G,et al.Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from750Ma to the present[J].Island Arc,1997,6:121-142
21汤良杰,贾承造,皮学军,等.库车前陆褶皱带盐相关构造样式[J].中国科学(D辑),2003,33(1):38～46
22Zhou J X,Xu F Y,Wang TC,et al.Cenozoic deformation histry of the Qaidam basin,NW China:results from cross-section restoration and implications for Qinghai-Tibet tectonics[J].Earth and Plane-tary Science Letters,2006,243:195-210
23彭文绪,周心怀,彭刚,等.渤海海域油气藏特征统计分析[J].中国海上油气,2008,20(1):18～21
2陆克政,漆家福,戴俊生.渤海湾新生代含油气盆地构造模式[J].北京:地质出版社,1997.251
3汤良杰,万桂梅,周新怀,等.渤海海域新生代构造演化[J].高校地质学报,2008,14(2):191～198
4侯贵廷,钱祥麟,蔡东升.渤海中、新生代盆地构造活动与沉积作用的时空关系[J].石油与天然气地质,2000,21(3):201～206
5Xiao H,Suppe J.Origin of rollover[J].AAPG Bulletin,1992,76:509-529
6葛建党.郯庐断裂在渤中凹陷的构造特征与油气成藏的关系[J].海洋石油,2001,(1):14～20
7刘和甫,李晓清,刘立群,等.伸展构造与裂谷盆地成藏区带[J].石油与天然气地质,2005,26(5):537～552
8漆家福,王德仁,陈书平,等.兰聊断层的几何学、运动学特征对东濮凹陷构造样式的影响[J].石油与天然气地质,2006,27(4):451～459
9邓津辉,周心怀,魏刚,等.郯庐走滑断裂带活动特征与油气成藏关系———以金县地区为例[J].石油与天然气地质,2008,29(1):102～105
10Rowan MG,Kligfield R.Cross section restoration and balancing as aid to seismic interpretion in extensional terranes[J].AAPG Bul-letin,1989,73(8):955-966
11White N J,Jackson J A,MeKenzie D P.The relationship between the geometry of normal faults and that of the sedimentary layers in their hanging walls[J].Journal of Structural Geology,1986,8:897-909
12Gibbs A.Development of extension and mixed-mode sedimentary basins,in continental extensional tectonics[A].In:Coward M P,Dewey J F,Hancock P L,eds.Geological Society Special Publica-tion London,1987,28:19-33
13Williams G,Vann I.The geometry of listric normal faults and de-formation in their hanging-walls[J].Journal of Structural Geology,1987,9:789-795
14Withjack M O,Gallaway S.Active normal faulting beneath a salt layer:an experimental study of deformation patterns in the cover sequence[J].AAPG Bulletin,2000,84(5):627-651
15余一欣,周心怀,汤良杰,等.渤海海域莱州湾凹陷KL112地区盐构造特征[J].地质学报,2008,82(6):731～737
16Lee T Y,Lawver L A.Cenozoic plate reconstruction of southeast Asia[J].Tectonophysics,1995,251:85-138
17Engebretson D C,Cox A,Gordon R G.Relative motions between oceanic and continental plates in the Pacific basin[J].The Geolo-gical Society of America Special Paper206,1985.1-59
18马杏垣,刘和甫,王维襄,等.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,1983,57(1):22～32
19漆家福,张一伟,陆克政,等.渤海湾新生代裂陷盆地的伸展模式及其动力学过程[J].石油实验地质,1995,17(4):316～323
20Maruyama S,Isozaki Y,Kimura G,et al.Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from750Ma to the present[J].Island Arc,1997,6:121-142
21汤良杰,贾承造,皮学军,等.库车前陆褶皱带盐相关构造样式[J].中国科学(D辑),2003,33(1):38～46
22Zhou J X,Xu F Y,Wang TC,et al.Cenozoic deformation histry of the Qaidam basin,NW China:results from cross-section restoration and implications for Qinghai-Tibet tectonics[J].Earth and Plane-tary Science Letters,2006,243:195-210
23彭文绪,周心怀,彭刚,等.渤海海域油气藏特征统计分析[J].中国海上油气,2008,20(1):18～21
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心