孙吴-嘉荫盆地中新生代构造特征及演化
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摘要
针对东北亚中新生代盆地构造演化具有复杂性和特殊性,依据对各种地质资料的综合解释与分析,剖析了孙吴-嘉荫盆地中新生代断裂特征,建立了一条横穿整个盆地的地震-地质区域大剖面,由此分析了盆地演化史.结果表明:孙吴-嘉荫盆地在宁远村组沉积时期,全盆地属于受北北东向伸展断裂控制的断陷盆地.淘淇河组沉积早期,盆地出现东西部的分异,东部表现为早期控陷断裂反转逆冲活动,此后进入了拗陷发育阶段,而此时西部仍为持续的断陷阶段;至淘淇河组沉积晚期,西部开始抬升剥蚀,东部为持续拗陷阶段.晚白垩世时盆地整体进入断陷后热沉降阶段;晚白垩世末盆地再次遭受挤压,形成典型的"下正上逆"正反转构造.新生代盆地进入挤压改造期,形成一系列以北西西向为主的具有压扭性质的右行走滑断裂.
Aimed at studying the complexity of tectonic evolution of the Mesozoic-Cenozoic basins in Northeast Asia in particular.Base on comprehensive interpretation and analyses of the geological and geophysical data,and constructed regional geological section across the basin,the Mesozoic and Cenozoic fault systems of the Sunwu-Jiayin basin were studied and the evolution of the basin discussed.The results show that the whole Sunwu-Jiayin basin is a faulted basin controlled by early Cretaceous NNE extensional faults that occurred during the deposition period of the Ningyuancun formation.The Jiayin region,which is located in the eastern part of the study area,was uplifted and suffered erosion during the early stage of the deposition period of the Taoqihe formation,while the Sunwu region in the western part remained to be a faulted basin.The Jiayin region evolved as a depression,whereas the Sunwu region was uplift and subjected to erosion during the late stage of the deposition period of the Taoqihe formation.Then the whole basin entered the depression phase due to the thermal subsidence after rifting,and received a wide deposition during the late Cretaceous.The basin suffered compression again at the end of the late Cretaceous,causing reactivation and reversion of the early faults.Since the Cenozoic,the compression stress has all along been existing in the study area,and a set of NWW-trending right-lateral transpressional strike-slip faults were thereby formed.
Aimed at studying the complexity of tectonic evolution of the Mesozoic-Cenozoic basins in Northeast Asia in particular.Base on comprehensive interpretation and analyses of the geological and geophysical data,and constructed regional geological section across the basin,the Mesozoic and Cenozoic fault systems of the Sunwu-Jiayin basin were studied and the evolution of the basin discussed.The results show that the whole Sunwu-Jiayin basin is a faulted basin controlled by early Cretaceous NNE extensional faults that occurred during the deposition period of the Ningyuancun formation.The Jiayin region,which is located in the eastern part of the study area,was uplifted and suffered erosion during the early stage of the deposition period of the Taoqihe formation,while the Sunwu region in the western part remained to be a faulted basin.The Jiayin region evolved as a depression,whereas the Sunwu region was uplift and subjected to erosion during the late stage of the deposition period of the Taoqihe formation.Then the whole basin entered the depression phase due to the thermal subsidence after rifting,and received a wide deposition during the late Cretaceous.The basin suffered compression again at the end of the late Cretaceous,causing reactivation and reversion of the early faults.Since the Cenozoic,the compression stress has all along been existing in the study area,and a set of NWW-trending right-lateral transpressional strike-slip faults were thereby formed.
引文
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[16]LIU M,CUI X,LIU F.Cenozoic rifting and volca-nism in eastern China:a mantle dynamic link to theIndo-Asian collision?[J].Tectonophysics,2004(393):39-42.
[17]YIN A.Cenozoic tectonic evolution of Asia:A pre-liminary synthesis[J].Tectonophysics,2010,488(1/4):293-325.
[18]ZHU G Z,SHI Y L,TACKLEY P.Subduction ofthe western Pacific Plate underneath northeast Chi-na:Implications of numerical studies[J].Physics ofthe Earth and Planetary Interiors,2010,277(1):244-252.
[19]郝天珧,刘伊克,段昶.中国东部及其邻域地球物理场特征与大地构造意义[J].地球物理学报,1997,40(5):108-116.HAO Tian-yao,LIU Yi-ke,DUAN Chang.Char-acteristics of geophysical field in east China and ad-jacent regions[J].Geoscience Journal,1997,40(5):108-116.
[20]FAURE M,NATAL′IN B.A,MONIE P,et al.Tectonic evolution of the Anuy metamorphic rocks(Sikhote Alin,Russia)and their place in the Meso-zoic geodynamic framework of East Asia[J].Tec-tonophysics,1995,241(3/4):279.
[21]张雷,刘招君,和钟铧,等.孙吴-嘉荫盆地白垩系淘淇河组-太平林场组砂岩主量元素的地球化学特征[J].沉积与特提斯地质,2008,28(2):100-106.ZHANG Lei,LIU Zhao-jun,HE Zhong-hua,et al.Geochemistry of major elements from the CretaceousTaoqihe Formation-Taipinglinchang Formationsandstones in the Sunwu-Jiayin bain[J].Sedimenta-ry Geology and Tethyan Geoloy,2008,28(2):100-106.
[22]赵海滨,尹志刚,汪岩,等.黑龙江北部嘉荫盆地中南部原划新近系时代的重新厘定[J].地质通报,2006,25(4):460-464.ZHAO Hai-bin,YIN Zhi-gang,WANG Yan,et al.The refine for neogene in the central and southern ofJiayin basin,in northern Heilongjiang[J].Geolog-ical Bulletin of Chian,2006,25(4):460-464.
[23]蒋甫玉,孟令顺,张凤旭,等.利用重力资料研究黑龙江省孙吴-嘉荫地区基底构造特征及油气远景[J].世界地质,2007,26(3):363-367.JIANG Fu-yu,MENG Ling-shun,ZHANG Feng-xu,et al.Study on characteristics of basal structureand oil-gas potential in Sunwu-Jiayin area of Hei-longjiang by using gravimetric data[J].Global Ge-logy,2007,26(3):363-367.
[24]CASTAING C,HALAWANI M.A,GERVAIS F,et al.Scaling relationships in intraplate fracture sys-tems related to Red Sea rifting[J].Tectonophysics,1996,261(4):291.
[25]COSENTINO D,RITA D,FUNICIELLO R,et al.Fracture system in Phlegraean Fields(Naples,southern Italy)[J].Bulletin Volcanologique,1984,47(2):247-257.
[26]卢华复,王胜利,罗俊成,等.塔里木盆地东部断裂系统及其构造演化[J].石油与天然气地质,2006,27(4):9.LU Hua-fu,WANG Sheng-li,LUO Jun-cheng,etal.Fault systems and their tectonic evolution in theeastern Tarim basin[J].Oil&Gas Geology,2006,27(4):9.
[27]罗群.中国东北地区断裂系统及其控藏特征[J].石油实验地质,2010(3):205-210.LUO Qun.Fault systems and characteristics oftheir controling reservior formation in the northeastChina[J].Petroleum Geology&Experiment,2010(3):205-210.
[28]CHEN P J,LI G,DAVID J B.Evolution,migra-tion and radiation of late Mesozoic conchostracans inEast Asia[J].Geological Journal,2007,42(3/4):391-413.
[29]周建波,张兴洲,马志红,等.中国东北地区的构造格局与盆地演化[J].石油与天然气地质,2009,30(5):530-538.ZHOU Jian-bo,ZHANG Xing-zhou,MA Zhi-hong,et al.Tectonic framework and basin evolu-tion in northeast China[J].Oil&Gas Geology,2009,30(5):530-538.
[30]谯汉生,方朝亮,牛嘉玉,等.东北地区深层石油地质[M].北京:石油工业出版社,2003:11-20.
[31]谢鸣谦.拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社,2000:1-21.
[32]李晓英,任凤和,张晓博,等.黑龙江省东部区域动力学环境分析[J].黄金科学技术,2008,16(2):24-28.LI Xiao-ying,REN Feng-he,ZHANG Qing-dao,etal.Analysis on geological dynamic condition in HeiLongjang Eastern Area[J].Gold Science and Tech-nology,2008,16(2):24-28.
[33]FANG S,ZHOU X R,LIU Z J,et al.Thrust e-vent of the provenances revealed by zircon fissiontrack ages in Tangyuan fault-basin,NE China[J].Radiation Measurements,2008,43(Supp 1):S324-S328.
[2]杨建国,邵曌一,吴河勇,等.黑龙江北部孙吴-嘉荫盆地沉积相类型及其演化[J].地质科学,2008,43(4):648-658.YANG Jian-guo,SHAO Zhao-yi,WU He-yong,etal.Sedimentaryfaciestypesand evolution of the Sun-wu-Jiayin basin in northern Heilongjiang province[J].Chinese Journal of Geology,2008,43(4):648-658.
[3]田梦.孙吴-嘉荫盆地地层序列、盆地演化及含油气远景[D].长春:吉林大学地球科学学院,2008.
[4]郑玉龙,刘文龙,乔秀云.黑龙江孙吴-嘉荫盆地白垩纪孢粉组合及地层划分对比[J].地层学杂志,2005,29(4):342-347.ZHANG Yu-long,LIU Wen-long,QIAO Xiu-Yun.Cretaceous sporo-pollen assemblages in Sunwu-Jiyinbasin and stratiraphic significance[J].Journal ofStratigraphy,2005,29(4):342-347.
[5]谯汉生,于兴河.裂谷盆地石油地质[M].北京:石油工业出版社,2004:26-31.
[6]KIRILLOVA G L.Late Mesozoic-Cenozoic sedimen-tary basins of active continental margin of SoutheastRussia:paleogeography,tectonics,and coal-oil-gaspresence[J].Marine and Petroleum Geology,2003,20(3/4):385-397.
[7]DUAN Y H,ZHAO D P,ZHANG X K,et al.Seis-mic structure and origin of active intraplate volcanoesin northeast Asia[J].Tectonophysics,2009,470(3/4):257-266.
[8]CHEN C H,LEE C Y,SHINJO R.Was there Ju-rassic Paleo-Pacific subduction in south China?:Con-straints from 40Ar/39Ar dating,elemental and Sr-Nd-Pb isotopic geochemistry of the Mesozoic basalts[J].Lithos,2008,183(1):9-39.
[9]HUANG J L,ZHAO D P.High-resolution mantletomography of China and surrounding regions[J].Journal of Geophysical Research-solid Earth,2006,111(B9):253-267.
[10]LIU J Q,HAN J T,FYFE W S.Cenozoic episodicvolcanism and continental rifting in northeast Chinaand possible link to Japan Sea development as re-vealed from K-Ar geochronology[J].Tectonophys-ics,2001,247(1):144-161.
[11]邵济安.中国东北地体与东北亚大陆边缘演化[M].北京:地震出版社,1995:171-176.
[12]孙文斌,和跃时.中国东北地区地震活动特征及其与日本海板块俯冲的关系[J].地震地质,2004,26(1):122-132.SUN Wen-bin,HE Yue-shi.The feature of seismic-ity in northeastern China and its relation to the sub-duction of the Japan sea plate[J].Seismology andGeology,2004,26(1):122-132.
[13]LI X Q,YUAN X H.Receiver functions in north-east China-implications for slab penetration into thelower mantle in northwest Pacific subduction zone[J].Earth and Planetary Science Letters,2003,239(1):9-17.
[14]张原庆,钱祥麟,李江海.板块碰撞远程效应的传播与地球层圈间的运动[J].地学前缘,2001,8(4):341-342.ZHANG Yuan-qin,QIAN Xiang-lin,LI Jiang-hai.The spread of long-range effects from plate collisionand the movement the earth's layers[J].Earth Sci-ence Frontiers,2001,8(4):341-342.
[15]REN J Y,TAMAKI K,LI S T,et al.Late Meso-zoic and Cenozoic rifting and its dynamic setting ineastern China and adjacent areas[J].Tectonophys-ics,2002,13(3):305-315.
[16]LIU M,CUI X,LIU F.Cenozoic rifting and volca-nism in eastern China:a mantle dynamic link to theIndo-Asian collision?[J].Tectonophysics,2004(393):39-42.
[17]YIN A.Cenozoic tectonic evolution of Asia:A pre-liminary synthesis[J].Tectonophysics,2010,488(1/4):293-325.
[18]ZHU G Z,SHI Y L,TACKLEY P.Subduction ofthe western Pacific Plate underneath northeast Chi-na:Implications of numerical studies[J].Physics ofthe Earth and Planetary Interiors,2010,277(1):244-252.
[19]郝天珧,刘伊克,段昶.中国东部及其邻域地球物理场特征与大地构造意义[J].地球物理学报,1997,40(5):108-116.HAO Tian-yao,LIU Yi-ke,DUAN Chang.Char-acteristics of geophysical field in east China and ad-jacent regions[J].Geoscience Journal,1997,40(5):108-116.
[20]FAURE M,NATAL′IN B.A,MONIE P,et al.Tectonic evolution of the Anuy metamorphic rocks(Sikhote Alin,Russia)and their place in the Meso-zoic geodynamic framework of East Asia[J].Tec-tonophysics,1995,241(3/4):279.
[21]张雷,刘招君,和钟铧,等.孙吴-嘉荫盆地白垩系淘淇河组-太平林场组砂岩主量元素的地球化学特征[J].沉积与特提斯地质,2008,28(2):100-106.ZHANG Lei,LIU Zhao-jun,HE Zhong-hua,et al.Geochemistry of major elements from the CretaceousTaoqihe Formation-Taipinglinchang Formationsandstones in the Sunwu-Jiayin bain[J].Sedimenta-ry Geology and Tethyan Geoloy,2008,28(2):100-106.
[22]赵海滨,尹志刚,汪岩,等.黑龙江北部嘉荫盆地中南部原划新近系时代的重新厘定[J].地质通报,2006,25(4):460-464.ZHAO Hai-bin,YIN Zhi-gang,WANG Yan,et al.The refine for neogene in the central and southern ofJiayin basin,in northern Heilongjiang[J].Geolog-ical Bulletin of Chian,2006,25(4):460-464.
[23]蒋甫玉,孟令顺,张凤旭,等.利用重力资料研究黑龙江省孙吴-嘉荫地区基底构造特征及油气远景[J].世界地质,2007,26(3):363-367.JIANG Fu-yu,MENG Ling-shun,ZHANG Feng-xu,et al.Study on characteristics of basal structureand oil-gas potential in Sunwu-Jiayin area of Hei-longjiang by using gravimetric data[J].Global Ge-logy,2007,26(3):363-367.
[24]CASTAING C,HALAWANI M.A,GERVAIS F,et al.Scaling relationships in intraplate fracture sys-tems related to Red Sea rifting[J].Tectonophysics,1996,261(4):291.
[25]COSENTINO D,RITA D,FUNICIELLO R,et al.Fracture system in Phlegraean Fields(Naples,southern Italy)[J].Bulletin Volcanologique,1984,47(2):247-257.
[26]卢华复,王胜利,罗俊成,等.塔里木盆地东部断裂系统及其构造演化[J].石油与天然气地质,2006,27(4):9.LU Hua-fu,WANG Sheng-li,LUO Jun-cheng,etal.Fault systems and their tectonic evolution in theeastern Tarim basin[J].Oil&Gas Geology,2006,27(4):9.
[27]罗群.中国东北地区断裂系统及其控藏特征[J].石油实验地质,2010(3):205-210.LUO Qun.Fault systems and characteristics oftheir controling reservior formation in the northeastChina[J].Petroleum Geology&Experiment,2010(3):205-210.
[28]CHEN P J,LI G,DAVID J B.Evolution,migra-tion and radiation of late Mesozoic conchostracans inEast Asia[J].Geological Journal,2007,42(3/4):391-413.
[29]周建波,张兴洲,马志红,等.中国东北地区的构造格局与盆地演化[J].石油与天然气地质,2009,30(5):530-538.ZHOU Jian-bo,ZHANG Xing-zhou,MA Zhi-hong,et al.Tectonic framework and basin evolu-tion in northeast China[J].Oil&Gas Geology,2009,30(5):530-538.
[30]谯汉生,方朝亮,牛嘉玉,等.东北地区深层石油地质[M].北京:石油工业出版社,2003:11-20.
[31]谢鸣谦.拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社,2000:1-21.
[32]李晓英,任凤和,张晓博,等.黑龙江省东部区域动力学环境分析[J].黄金科学技术,2008,16(2):24-28.LI Xiao-ying,REN Feng-he,ZHANG Qing-dao,etal.Analysis on geological dynamic condition in HeiLongjang Eastern Area[J].Gold Science and Tech-nology,2008,16(2):24-28.
[33]FANG S,ZHOU X R,LIU Z J,et al.Thrust e-vent of the provenances revealed by zircon fissiontrack ages in Tangyuan fault-basin,NE China[J].Radiation Measurements,2008,43(Supp 1):S324-S328.
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