胶莱盆地深部拆离系统及其区域构造意义
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摘要
地震剖面解释结果揭示了胶莱盆地深部两个低角度拆离断裂系统:一个发育于盆地南部诸城凹陷,主拆离面向南缓倾,深度为8~10 km;另一个发育于盆地北部高密凹陷和莱阳凹陷深部,由一系列北倾犁式正断层组成,主拆离面向北或北北东缓倾。根据受控凹陷的地层记录分析、剖面复原分析和伸展量估算,并结合地表断裂滑动矢量反演结果,认为盆地南部拆离系统主要形成于早白垩世莱阳组沉积时期,该时期诸城凹陷南北向伸展量达36%~41%,最大伸展方向可能为北西-南东。该拆离系统继承了早期胶南(或苏鲁)造山带深部滑脱构造面,其后期拆离复活主导了胶莱盆地南部不对称伸展构造样式,控制了狭长展布的莱阳期沉积凹陷发育。北部拆离系统主要形成于晚白垩世盆地伸展阶段,伸展作用可能延续到古新世时期,控制了盆地王氏组沉积。这个时期横穿莱阳凹陷和高密凹陷南北向伸展量估计为20%~25%,最大的伸展方向近南北向。该拆离系统调节了胶莱盆地近南北向拉分伸展,其形成与盆地东、西两侧北北东向边界断裂带右旋剪切作用有关。胶莱盆地深部两个深部拆离系统的时空复合或叠合造就了盆地内部复杂的伸展构造样式。识别这两个拆离系统不仅对盆地形成机理和动力学背景提供了重要的深部构造制约,对盆地油气勘探也具有重要的指导意义。
Seismic interpretations reveal two low angle detachment systems in the Jiaolai basin: one,developed(8~10) km beneath the Zhucheng depression in the southern part of the basin,has a detachment surface gently dipping to the south; the other,developed in the north Gaomi and Laiyang depressions,consists of a series of N-dipping listric normal faults and has a major detachment surface gently dipping to the north or NNE.Based on the sed-imentary records analysis,profile retro-deformation,and estimated stretch properties of the above-mentioned depressions,in combination with the fault slip data analyses at the surface,the southern detachment system is considered to be formed during the early Cretaceous Laiyang stage when the Zhucheng depression had a N-S stretching rate of 36%~41% and a possible NW-SE maximum stretching.This detachment system inherited an early deep decollement zone in the Jiaonan(or Su-Lu) orogenic belt;its late reactivation dominated the asymmetric extension pattern and controlled the development of the narrow,elongate sedimentary depression in the Jiaolai basin in Laiyang stage.The northern detachment system had taken shape during the stretching stage in the late Cretaceous.It is possible that the stretching process continued until the Paleocene and controlled the deposition of the Wangshi Formations.The N-S extension across the Laiyang and Gaomi depressions during the stage is estimated to be at(20%~)25%,the maximum stretching direction being nearly N-S.This detachment system accommodated the N-S pull-apart stretching of Jiaolai basin and its formation was related to the right-lateral shear along the NNE-trending boundary fault zones on the eastern and western sides of the basin.The spatial and temporal superimposition of these two detachment systems resulted in the complex extensional structural styles in the Jiaolai basin.The identification of these two deep detachment systems not only provides structural constraints on the mechanisms and dynamic setting of the basin formation,but also is of great significance for petroleum exploration in the basin.
Seismic interpretations reveal two low angle detachment systems in the Jiaolai basin: one,developed(8~10) km beneath the Zhucheng depression in the southern part of the basin,has a detachment surface gently dipping to the south; the other,developed in the north Gaomi and Laiyang depressions,consists of a series of N-dipping listric normal faults and has a major detachment surface gently dipping to the north or NNE.Based on the sed-imentary records analysis,profile retro-deformation,and estimated stretch properties of the above-mentioned depressions,in combination with the fault slip data analyses at the surface,the southern detachment system is considered to be formed during the early Cretaceous Laiyang stage when the Zhucheng depression had a N-S stretching rate of 36%~41% and a possible NW-SE maximum stretching.This detachment system inherited an early deep decollement zone in the Jiaonan(or Su-Lu) orogenic belt;its late reactivation dominated the asymmetric extension pattern and controlled the development of the narrow,elongate sedimentary depression in the Jiaolai basin in Laiyang stage.The northern detachment system had taken shape during the stretching stage in the late Cretaceous.It is possible that the stretching process continued until the Paleocene and controlled the deposition of the Wangshi Formations.The N-S extension across the Laiyang and Gaomi depressions during the stage is estimated to be at(20%~)25%,the maximum stretching direction being nearly N-S.This detachment system accommodated the N-S pull-apart stretching of Jiaolai basin and its formation was related to the right-lateral shear along the NNE-trending boundary fault zones on the eastern and western sides of the basin.The spatial and temporal superimposition of these two detachment systems resulted in the complex extensional structural styles in the Jiaolai basin.The identification of these two deep detachment systems not only provides structural constraints on the mechanisms and dynamic setting of the basin formation,but also is of great significance for petroleum exploration in the basin.
引文
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3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):537~552L iu Hefu,L i X iaoq ing,L iu L iqun,et al.Petroleum plays in rift ba-sins and extensional structures[J].O il&Gas Geology,2005,26(5):537-552
4 W ern icke B,Burchfiel B C.Modes of extensional tecton ics[J].Journal of Structruai Geolology 1982,4:105-113
5 Buck W R,Martinez F,Steckler M S,et al.Thermal conse-quences of lithospheric extension:pure and simple[J].Tecton-ics,1988,7(2):213-234
6 Reston T J,Ruoff O,M cB ride J H,et al.D etachm ent and steepnormal fau lting in Atlantic ocean ic crustwest ofA frica[J].Geol-ogy,1996,24(9):811-814
7 W oldai Ghebreab.Tecton ics of the Red Sea region reassessed[J].Earth-Science Reviews,1998,45:1-44
8 Collettin i C,Barch iM R.A low angle normal fau lt in the Umbriaregion(Central Italy):a m echan icalmodel for the related m icro-seism icity[J].Tectonophysics,2002,359:97-115
9张晓东,余青,陈发景,等.松辽盆地变质核杂岩和伸展断陷的构造特征及成因[J].地学前缘,2000,7(4):411~419Zhang X iaodong,Yu Q ing,Chen Fajing,et al.Structural charac-teristics,origin and evolution ofm etamorph ic core complex in cen-tral basem ent uplift and Xu jiaweizi fau lted depression in Songliaobasin,northeast Ch ina[J].Earth Science Frontiers,2000,7(4):411-419
10黄泽光,高长林,吉让寿.南华北地区中新生代盆地演化[J].石油与天然气地质,2005,26(2):252~256Huang Zeguang,Gao Changlin,Ji Rangshou.Analysis of evolu-tion ofM eso-Cenozoic basins in southern North Ch ina[J].O il&Gas Geology,2005,26(2):252-256
11刘池洋.后期改造强烈———中国沉积盆地重要特点之一[J].石油与天然气地质,1996,17(4):255~261L iu Ch iyang.Strong late-reformation:one of the important char-acteristics of sed im entary basins in Ch ina[J].O il&Gas Geolo-gy,1996,17(4):255-261
12陆克政,戴俊生.胶莱盆地的形成和演化[M].山东东营:石油大学出版社,1994.1~174Lu Kezheng,Dai Junsheng.Evolution of Jiaolai pu ll-apart basin[M].Shandong Dongying:Petroleum Un iversity Pub lish ingHouse,1994.1-174
13任纪舜.从全球看中国大地构造[M].北京:地质出版社,1999.1~15Ren Jishun.Ch ina tecton ics in the light of global[M].Beijing:Geological Pub lish ing House,1999.1-15
14贾东,何永明,施央申,等.山东地体构造及其拼贴运动学研究[M].南京:南京大学出版社,1993.1~100Jia Dong,He Yongm ing,Sh i Yangshen,et al.Stud ies on theShandong terrane:tecton ics and its k inematics of terrane collage[M].Nan jing:Pub lish ingHouse ofNan jingUn iversity,1993.1-100
15张建新,杨天南,许志琴,等.胶南地区的伸展作用———以胶南-诸城一带为例[J].地球学报,1997,18(2):122~128Zhang Jianxin,Yang Tiannan,Xu Zh iq in,et al.Extension of Jia-onan area in Shandong[J].Acta Geoscientia S in ica,1997,18(2):122-128
16蔡乾忠.横贯黄海的中朝造山带与北、南黄海成盆成烃关系[J].石油与天然气地质,2005,26(2):185~192,196Cai Q ianzhong.Relationsh ip between S ino-Korean orogen ic belttraversing Yellow Sea and basin evolution and hydrocarbon genera-tion in North and South Yellow Sea basins[J].O il&Gas Geolo-gy,2005,26(2):185-192,196
17郑求根,蔡立国,丁文龙,等.黄海海域盆地的形成与演化[J].石油与天然气地质,2005,26(5):647~654Zheng Q iugen,Cai L iguo,D ing W en long,et al.D evelopm ent andevolution of basins in Yellow Sea[J].O il&Gas Geology,2005,26(5):647-654
18李桂群,范德江,任景明.胶莱盆地发育演化及其油气前景探讨[J].青岛海洋大学学报,1994,24(3):413~419L i Gu iqun,Fan D ejiang,Ren Jingm ing.The evolution features ofthe Jiaolai basin and study of its prospective oil and gas deposits[J].Journal ofOcean Un iversity ofQ ingdao,1994,24(3):413-419
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