南黄海千里岩附近海域第四纪构造活动特征
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摘要
南黄海千里岩附近海域是千里岩隆起区地震活动较强烈的区域,对该区域新近获得的单道地震剖面的分析表明,海底第四纪沉积层中发育较多的褶皱和断层构造,断层以逆断层为主,褶皱则主要为平缓斜歪褶皱,为断层活动引起.褶皱和断层构造多形成于中更新世以前,千里岩断裂等部分断层最新活动至晚更新世,且具有生长断层的特征,反映了区域较强的活动性.研究区新近纪-中更新世的构造变形可能与南黄海最新一期构造运动有关,是区域构造应力场变化的产物.
Many Quaternary folds and faults are identified on the seismic reflection profiles acquired in the adjacent areas of Qianliyan Island of southern Yellow Sea.The faults are mainly of reverse fault.The folds are mainly gentle and tilted,caused by fault activities.Most folds and faults occurred below a plane of unconformity between middle Pleistocene and its overlying upper Pleistocene.Some faults,such as Qianliyan fault,are late Pleistocene active fault.Many faults and folds were synsedimentarily developed in the lower Pleistocene and underlying strata,revealling rather strong tectonic activity,especially at the basin boundary where the faults even cut into the late Pleistocene stratum.The formation of folds and faults was attributed to the last tectogenesis of the Yellow Sea in middle Pleistocene,which maybe correspond to the Kunlun-Huanghe movement of Qinghai-Tibet plateau.At that time,the N-S striking horizontal stress drove the early-developed basin boundary faults reactive and further induced the NEE or E-W striking tectonic deformation in the overlying sedimentary layer.
Many Quaternary folds and faults are identified on the seismic reflection profiles acquired in the adjacent areas of Qianliyan Island of southern Yellow Sea.The faults are mainly of reverse fault.The folds are mainly gentle and tilted,caused by fault activities.Most folds and faults occurred below a plane of unconformity between middle Pleistocene and its overlying upper Pleistocene.Some faults,such as Qianliyan fault,are late Pleistocene active fault.Many faults and folds were synsedimentarily developed in the lower Pleistocene and underlying strata,revealling rather strong tectonic activity,especially at the basin boundary where the faults even cut into the late Pleistocene stratum.The formation of folds and faults was attributed to the last tectogenesis of the Yellow Sea in middle Pleistocene,which maybe correspond to the Kunlun-Huanghe movement of Qinghai-Tibet plateau.At that time,the N-S striking horizontal stress drove the early-developed basin boundary faults reactive and further induced the NEE or E-W striking tectonic deformation in the overlying sedimentary layer.
引文
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Cui,Z.J.,Wu,Y.Q.,Liu,G.N.,1997.Discovery and character of Kunlun-Huanghe movement.ChineseScience Bulletin,42(18):1986-1989(in Chinese).
Fu,Y.T.,Yu,Z.Y.,2010.Metamorphosed marine clastic rocks in Qingdao:tectonic attribute and implication.Chinese Journal of Geology,45(1):207-227(in Chinese with English abstract).
Ge,X.H.,Ren,S.M.,Ma,L.X.,et al.,2006.Multi-stage uplifts of the Qinghai-Tibet plateau and their environ-mental effects.Earth Science Frontiers,13(6):118-130(in Chinese with English abstract).
Gong,Z.S.,2004.Neotectonics and petroleum accumulation in offshore Chinese basins.Earth Science—Journal of China University of Geosciences,29(5):513-517(in Chinese with English abstract).
Gu,G.X.,1983.Earthquake catalogue of China.Science Press,Beijing(in Chinese).
Guo,Y.G.,1997.Geological structure features of Yellow Sea,East China Sea and adjacent areas.In:Xu,D.T.,Liu,X.Q.,Zhang,X.H.,et al.,eds.,China offshore geology.Geological Publishing House,Beijing,223-229(in Chinese).
He,Z.Q.,Chen,Y.K.,Ye,T.L.,et al.,2007.Application of shallow seismic exploration in detection of buried fault in coastal areas.Seismology and Geology,29(2):363-372(in Chinese with English abstract).
Jia,C.Z.,He,D.F.,Lu,J.M.,2004.Episodes and geodynamic setting of Himalayan movement in China.Oil&Gas Geology,25(2):121-125(in Chinese with English abstract).
Liu,G.D.,1992.The geological and geophysical map of the Chinas seas and adjacent areas(1∶5 000 000).Geological Publishing House,Beijing(in Chinese).
Luan,G.Z.,Ren,L.C.,Duan,B.C.,1999.Activity of NE and NW faults in Qingdao area and its neighbourhood.Journal of Ocean University of Qingdao,29(4):727-732(in Chinese with English abstract).
Qin,Y.S.,Zhao,Y.Y.,Zhao,L.R.,et al.,1989.Geology of the Huanghai Sea.Ocean Press,Beijing(in Chinese).
Song,C.H.,Gao,D.L.,Fang,X.M.,et al.,2005.Late Ce-nozoic high-resolution magnetostratigraphy in the Kun-lun Pass basin and its implications for the uplift of the northern Tibetan plateau.Chinese Science Bulletin,50(17):1912-1922.
Wan,T.F.,1994.Tectonic event and stress field of Quaternary in China.Quaternary Sciences,(1):48-55(in Chinese with English abstract).
Wan,T.F.,2004.Summary of China geotectonics.Geological Publishing House,Beijing(in Chinese).
Wan,T.F.,Cao,R.P.,1992.Tectonic events and stress fields of middle Eocene-Early Pleistocene in China.Geoscience,6(3):275-285(in Chinese with English abstract).
Wan,T.F.,Cao,X.H.,1997.Estimation of differential stress magnitude in middle-late Triassic to Early Pleistocene for China.Earth Science—Journal of China University of Geosciences,22(2):145-152(in Chinese with English abstract).
Wan,T.F.,Hao,T.Y.,2009.Cenozoic tectonics of the Yellow Sea and its oil-gas exploration.Geoscience,23(3):385-393(in Chinese with English abstract).
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Xu,Z.Q.,Qi,X.X.,Yang,J.S.,et al.,2006.Deep subduc-tion erosion model for continent-continent collision of the Sulu HP-UHP metamorphic terrain.Earth Sci-ence—Journal of China University of Geosciences,31(4):427-436(in Chinese with English abstract).
Yang,W.C.,Xu,J.R.,Cheng,Z.Y.,et al.,2005.Regional geophysics and crust-mantle interaction in Sulu-Dabie orogenic belt.Geological Publishing House,Beijing(in Chinese).
Yang,Z.G.,1993.The sedimentary sequence and palaeogeographic changes of the South Yellow Sea since the Olduvai subchron.Acta Geologica Sinica,67(4):357-366(in Chinese with English abstract).
Yao,Y.J.,Feng,Z.Q.,Hao,T.Y.,et al.,2008.A new understanding of the structural layers in the South Yellow Sea basin and their hydrocarbon-bearing characteristics.Earth Science Frontiers,15(6):232-240(in Chinese with English abstract).
Zhan,W.H.,Zhu,Z.Y.,Sun,L.T.,et al.,2006.The Epoch and diversities of neotectonic movement in the South China Sea.Acta Geologica Sinica,80(4):491-496(in Chinese with English abstract).
Zhang,X.H.,2008.Tectonic geology in China seas.Ocean Press,Beijing(in Chinese).
Zheng,G.Y.,1991.Quaternary geology in the Yellow Sea.Science Press,Beijing(in Chinese).
Zheng,Y.P.,Liu,B.H.,Wu,J.L.,et al.,2003.Characteristics of seismostratigraphy and analysis of structurallithofacies in the southern Yellow Sea Cenozoic basin.Chinese Science Bulletin,48(Supp.):56-63.
Zhou,H.Y.,2000.Environmental events and catastrophes from the end of Early Pleistocene to the early stage of Middle Pleistocene.Journal of Natural Disasters,9(2):123-129(in Chinese with English abstract).
Zhu,Z.Y.,Xie,J.B.,Zheng,W.Q.,et al.,2006.Neotectonics along the north coast of South China Sea and its regional correlation around the boundary of the Early and Middle Pleistocen.Quaternary Sciences,26(1):70-76(in Chinese with English abstract).
蔡东升,罗毓辉,武文来,等,2001.渤海浅层构造变形特征、成因机理与渤中坳陷及其周围油气富集的关系.中国海上油气(地质),15(1):35-43.
崔之久,吴永秋,刘耕年,1997.昆仑-黄河运动的发现及其性质.科学通报,42(18):1986-1989.
付永涛,虞子冶,2010.青岛垭口-八仙墩变质海相碎屑岩的属性和构造意义.地质科学,45(1):207-227.
葛肖虹,任收麦,马立祥,等,2006.青藏高原多期次隆升的环境效应.地学前缘,13(6):118-130.
龚再升,2004.中国近海含油气盆地新构造运动与油气成藏.地球科学——中国地质大学学报,29(5):513-517.
顾功叙,1983.中国地震目录.北京:科学出版社.
郭玉贵,1997.黄海、东海及邻域地质构造特征.见:许东禹,刘锡清,张训华,等编,中国近海地质.北京:地质出版社,223-229.
何正勤,陈宇坤,叶太兰,等,2007.浅层地震勘探在沿海地区隐伏断层探测中的应用.地震地质,29(2):363-372.
贾承造,何登发,陆洁民,2004.中国喜马拉雅运动的期次及其动力学背景.石油与天然气地质,25(2):121-125.
刘光鼎,1992.中国海区及邻域地质地球物理系列图(1∶500万).北京:地质出版社.
栾光忠,任鲁川,段本春,1999.青岛及其邻区NE、NW向断裂的活动性研究.青岛海洋大学学报,29(4):727-732.
秦蕴珊,赵一阳,赵丽蓉,等,1989.黄海地质.北京:海洋出版社.
宋春晖,高东林,方小敏,等,2005.青藏高原昆仑山垭口盆地晚新生代高精度磁性地层及其意义.科学通报,50(19):2145-2154.
万天丰,1994.中国第四纪的构造事件与应力场.第四纪研究,(1):48-55.
万天丰著,2004.中国大地构造学纲要.北京:地质出版社.
万天丰,曹瑞萍,1992.中国中始新世-早更新世构造事件与应力场.现代地质,6(3):275-285.
万天丰,曹秀华,1997.中国三叠纪中晚期-早更新世构造应力值的估算.地球科学———中国地质大学学报,22(2):145-152.
万天丰,郝天珧,2009.黄海新生代构造及油气勘探前景.现代地质,23(3):385-393.
王志才,晁洪太,杜宪宋,等,2008.南黄海北部千里岩断裂活动性初探.地震地质,30(1):176-186.
吴戈,2004.黄海及其邻区的历史地震.中国地震,20(3):299-305.
许志琴,戚学祥,杨经绥,等,2006.苏鲁高压-超高压变质地体的陆-陆碰撞深俯冲剥蚀模式.地球科学———中国地质大学学报,31(4):427-436.
许忠淮,吴少武,1997.南黄海和东海地区现代构造应力场特征的研究.地球物理学报,40(6):773-781.
杨文采,徐纪人,程振炎,等,2005.苏鲁大别造山带地球物理与壳幔作用.北京:地质出版社.
杨子赓,1993.Olduvai亚时以来南黄海沉积层序及古地理变迁.地质学报,67(4):357-366.
姚永坚,冯志强,郝天珧,等,2008.对南黄海盆地构造层特征及含油气性的新认识.地学前缘,15(6):232-240.
詹文欢,朱照宇,孙龙涛,等,2006.试论南海新构造运动的时限及其差异性.地质学报,80(4):491-496.
张训华,2008.中国海域构造地质学.北京:海洋出版社.
郑光膺,1991.黄海第四纪地质.北京:科学出版社.
郑彦鹏,刘保华,吴金龙,等,2001.南黄海新生代盆地地震地层特征及其构造岩相分析.科学通报,46(增刊):52-58.
周厚云,2000.早更新世末中更新世早期的环境事件与灾变.自然灾害学报,9(2):123-129.
朱照宇,谢久兵,郑王琼,等,2006.南海北缘早-中更新世之交新构造活动及其区域对比.第四纪研究,26(1):70-76.
Cui,Z.J.,Wu,Y.Q.,Liu,G.N.,1997.Discovery and character of Kunlun-Huanghe movement.ChineseScience Bulletin,42(18):1986-1989(in Chinese).
Fu,Y.T.,Yu,Z.Y.,2010.Metamorphosed marine clastic rocks in Qingdao:tectonic attribute and implication.Chinese Journal of Geology,45(1):207-227(in Chinese with English abstract).
Ge,X.H.,Ren,S.M.,Ma,L.X.,et al.,2006.Multi-stage uplifts of the Qinghai-Tibet plateau and their environ-mental effects.Earth Science Frontiers,13(6):118-130(in Chinese with English abstract).
Gong,Z.S.,2004.Neotectonics and petroleum accumulation in offshore Chinese basins.Earth Science—Journal of China University of Geosciences,29(5):513-517(in Chinese with English abstract).
Gu,G.X.,1983.Earthquake catalogue of China.Science Press,Beijing(in Chinese).
Guo,Y.G.,1997.Geological structure features of Yellow Sea,East China Sea and adjacent areas.In:Xu,D.T.,Liu,X.Q.,Zhang,X.H.,et al.,eds.,China offshore geology.Geological Publishing House,Beijing,223-229(in Chinese).
He,Z.Q.,Chen,Y.K.,Ye,T.L.,et al.,2007.Application of shallow seismic exploration in detection of buried fault in coastal areas.Seismology and Geology,29(2):363-372(in Chinese with English abstract).
Jia,C.Z.,He,D.F.,Lu,J.M.,2004.Episodes and geodynamic setting of Himalayan movement in China.Oil&Gas Geology,25(2):121-125(in Chinese with English abstract).
Liu,G.D.,1992.The geological and geophysical map of the Chinas seas and adjacent areas(1∶5 000 000).Geological Publishing House,Beijing(in Chinese).
Luan,G.Z.,Ren,L.C.,Duan,B.C.,1999.Activity of NE and NW faults in Qingdao area and its neighbourhood.Journal of Ocean University of Qingdao,29(4):727-732(in Chinese with English abstract).
Qin,Y.S.,Zhao,Y.Y.,Zhao,L.R.,et al.,1989.Geology of the Huanghai Sea.Ocean Press,Beijing(in Chinese).
Song,C.H.,Gao,D.L.,Fang,X.M.,et al.,2005.Late Ce-nozoic high-resolution magnetostratigraphy in the Kun-lun Pass basin and its implications for the uplift of the northern Tibetan plateau.Chinese Science Bulletin,50(17):1912-1922.
Wan,T.F.,1994.Tectonic event and stress field of Quaternary in China.Quaternary Sciences,(1):48-55(in Chinese with English abstract).
Wan,T.F.,2004.Summary of China geotectonics.Geological Publishing House,Beijing(in Chinese).
Wan,T.F.,Cao,R.P.,1992.Tectonic events and stress fields of middle Eocene-Early Pleistocene in China.Geoscience,6(3):275-285(in Chinese with English abstract).
Wan,T.F.,Cao,X.H.,1997.Estimation of differential stress magnitude in middle-late Triassic to Early Pleistocene for China.Earth Science—Journal of China University of Geosciences,22(2):145-152(in Chinese with English abstract).
Wan,T.F.,Hao,T.Y.,2009.Cenozoic tectonics of the Yellow Sea and its oil-gas exploration.Geoscience,23(3):385-393(in Chinese with English abstract).
Wang,Z.C.,Chao,H.T.,Du,X.S.,et al.,2008.Preliminary survey on the Quaternary activities of the Qianliyan fault in the northern part of the South Yellow Sea.Seismology and Geology,30(1):176-186(in Chinese with English abstract).
Wu,G.,2004.Historical earthquakes occurred in the Yellow Sea and its adjacent area.Earthquake Research in China,20(3):299-305(in Chinese with English abstract).
Xu,P.F.,Liu,F.T.,Ye,K.,et al.,2002.Flake tectonics in the Sulu orogen in eastern China as revealed by seismic tomography.Geophysical Research Letters,29(10):1385.doi:10.1029/2001GL014185
Xu,Z.H.,Wu,S.W.,1997.A study on present-day tectonic stress in the southern Yellow Sea and East China Sea region.Acta Geophysica Sinica,40(6):773-781(in Chinese with English abstract).
Xu,Z.Q.,Qi,X.X.,Yang,J.S.,et al.,2006.Deep subduc-tion erosion model for continent-continent collision of the Sulu HP-UHP metamorphic terrain.Earth Sci-ence—Journal of China University of Geosciences,31(4):427-436(in Chinese with English abstract).
Yang,W.C.,Xu,J.R.,Cheng,Z.Y.,et al.,2005.Regional geophysics and crust-mantle interaction in Sulu-Dabie orogenic belt.Geological Publishing House,Beijing(in Chinese).
Yang,Z.G.,1993.The sedimentary sequence and palaeogeographic changes of the South Yellow Sea since the Olduvai subchron.Acta Geologica Sinica,67(4):357-366(in Chinese with English abstract).
Yao,Y.J.,Feng,Z.Q.,Hao,T.Y.,et al.,2008.A new understanding of the structural layers in the South Yellow Sea basin and their hydrocarbon-bearing characteristics.Earth Science Frontiers,15(6):232-240(in Chinese with English abstract).
Zhan,W.H.,Zhu,Z.Y.,Sun,L.T.,et al.,2006.The Epoch and diversities of neotectonic movement in the South China Sea.Acta Geologica Sinica,80(4):491-496(in Chinese with English abstract).
Zhang,X.H.,2008.Tectonic geology in China seas.Ocean Press,Beijing(in Chinese).
Zheng,G.Y.,1991.Quaternary geology in the Yellow Sea.Science Press,Beijing(in Chinese).
Zheng,Y.P.,Liu,B.H.,Wu,J.L.,et al.,2003.Characteristics of seismostratigraphy and analysis of structurallithofacies in the southern Yellow Sea Cenozoic basin.Chinese Science Bulletin,48(Supp.):56-63.
Zhou,H.Y.,2000.Environmental events and catastrophes from the end of Early Pleistocene to the early stage of Middle Pleistocene.Journal of Natural Disasters,9(2):123-129(in Chinese with English abstract).
Zhu,Z.Y.,Xie,J.B.,Zheng,W.Q.,et al.,2006.Neotectonics along the north coast of South China Sea and its regional correlation around the boundary of the Early and Middle Pleistocen.Quaternary Sciences,26(1):70-76(in Chinese with English abstract).
蔡东升,罗毓辉,武文来,等,2001.渤海浅层构造变形特征、成因机理与渤中坳陷及其周围油气富集的关系.中国海上油气(地质),15(1):35-43.
崔之久,吴永秋,刘耕年,1997.昆仑-黄河运动的发现及其性质.科学通报,42(18):1986-1989.
付永涛,虞子冶,2010.青岛垭口-八仙墩变质海相碎屑岩的属性和构造意义.地质科学,45(1):207-227.
葛肖虹,任收麦,马立祥,等,2006.青藏高原多期次隆升的环境效应.地学前缘,13(6):118-130.
龚再升,2004.中国近海含油气盆地新构造运动与油气成藏.地球科学——中国地质大学学报,29(5):513-517.
顾功叙,1983.中国地震目录.北京:科学出版社.
郭玉贵,1997.黄海、东海及邻域地质构造特征.见:许东禹,刘锡清,张训华,等编,中国近海地质.北京:地质出版社,223-229.
何正勤,陈宇坤,叶太兰,等,2007.浅层地震勘探在沿海地区隐伏断层探测中的应用.地震地质,29(2):363-372.
贾承造,何登发,陆洁民,2004.中国喜马拉雅运动的期次及其动力学背景.石油与天然气地质,25(2):121-125.
刘光鼎,1992.中国海区及邻域地质地球物理系列图(1∶500万).北京:地质出版社.
栾光忠,任鲁川,段本春,1999.青岛及其邻区NE、NW向断裂的活动性研究.青岛海洋大学学报,29(4):727-732.
秦蕴珊,赵一阳,赵丽蓉,等,1989.黄海地质.北京:海洋出版社.
宋春晖,高东林,方小敏,等,2005.青藏高原昆仑山垭口盆地晚新生代高精度磁性地层及其意义.科学通报,50(19):2145-2154.
万天丰,1994.中国第四纪的构造事件与应力场.第四纪研究,(1):48-55.
万天丰著,2004.中国大地构造学纲要.北京:地质出版社.
万天丰,曹瑞萍,1992.中国中始新世-早更新世构造事件与应力场.现代地质,6(3):275-285.
万天丰,曹秀华,1997.中国三叠纪中晚期-早更新世构造应力值的估算.地球科学———中国地质大学学报,22(2):145-152.
万天丰,郝天珧,2009.黄海新生代构造及油气勘探前景.现代地质,23(3):385-393.
王志才,晁洪太,杜宪宋,等,2008.南黄海北部千里岩断裂活动性初探.地震地质,30(1):176-186.
吴戈,2004.黄海及其邻区的历史地震.中国地震,20(3):299-305.
许志琴,戚学祥,杨经绥,等,2006.苏鲁高压-超高压变质地体的陆-陆碰撞深俯冲剥蚀模式.地球科学———中国地质大学学报,31(4):427-436.
许忠淮,吴少武,1997.南黄海和东海地区现代构造应力场特征的研究.地球物理学报,40(6):773-781.
杨文采,徐纪人,程振炎,等,2005.苏鲁大别造山带地球物理与壳幔作用.北京:地质出版社.
杨子赓,1993.Olduvai亚时以来南黄海沉积层序及古地理变迁.地质学报,67(4):357-366.
姚永坚,冯志强,郝天珧,等,2008.对南黄海盆地构造层特征及含油气性的新认识.地学前缘,15(6):232-240.
詹文欢,朱照宇,孙龙涛,等,2006.试论南海新构造运动的时限及其差异性.地质学报,80(4):491-496.
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