沧县隆起献县变质核杂岩的发育特征及成因模式
|
摘要
渤海湾盆地周缘发育的多个变质核杂岩,很好地记录了华北克拉通东部晚中生代以来的地壳伸展过程。文中以渤海湾盆地西部献县凸起和饶阳凹陷为研究区,试图揭示盆地内部变质核杂岩的发育特征。根据井、震结合的方法,通过精细的构造解释,厘定了献县断层及其上盘的构造变形特征;利用凹陷内的钻井资料对献县凸起上发育地层的时代和岩性进行限定;结合区域上变质核杂岩的发育特征和形成背景,讨论了献县变质核杂岩的发育时间和成因演化模式。结果表明:在研究区内呈弧形展布的献县断层具有主拆离断层的特征,断层上盘的饶阳凹陷南部残留有中元古界和下古生界,且凹陷内发育有数量众多、不同倾向的次级断层;献县凸起上发育的地层为太古宇-古元古界,岩性包括角闪片麻岩、黑云二长片麻岩,局部发育有花岗片麻岩。研究认为,献县变质核杂岩具有典型变质核杂岩的基本特征,其形成时间为晚中生代(K1?),发育于华北克拉通东部岩石圈大规模减薄的背景下,并以滚动枢纽模式发展演化。
A series of metamorphic core complexes developed around the Bohai Bay Basin recording the crustal stretching process of the eastern North China Craton since the Late Mesozoic.In order to reveal the characteristics of the metamorphic core complex developed in the basin,we selected the Xianxian High and southern Raoyang Sag as the study area.We determined the deformation characteristics of the Xianxian fault and its hanging wall through fine interpretation of the seismic and drilling data,and constructed the age and lithology of the strata developed on the Xianxian High using drilling data obtained from the southern Raoyang Sag.We discuss here the timing and genetic model of the Xianxian metamorphic core complex based on comprehensive consideration of its developmental characteristics and background in the North China Craton.Our study shows that(1)the curved Xianxian fault in the study area has the characteristics of the main detachment fault;(2)the southern Raoyang Sag,located in the hanging wall of the fault,shows residual Middle Proterozoic to Lower Paleozoic accompanied by numerous secondary faults with different dips in the sag;and(3)the Archean to Paleoproterozoic strata constitute the main part of the Xianxian High with lithology including hornblende,biotite monzonitic and localized granite gneisses.Overall,our results demonstrate that the Xianxian metamorphic core complex,formed in the Late Mesozoic(K1?),has the basic characteristics of a typical metamorphic core complex.It developed in the background of the largescale lithospheric thinning of the eastern North China Craton and evolved in accordance with the rollinghinge model.
A series of metamorphic core complexes developed around the Bohai Bay Basin recording the crustal stretching process of the eastern North China Craton since the Late Mesozoic.In order to reveal the characteristics of the metamorphic core complex developed in the basin,we selected the Xianxian High and southern Raoyang Sag as the study area.We determined the deformation characteristics of the Xianxian fault and its hanging wall through fine interpretation of the seismic and drilling data,and constructed the age and lithology of the strata developed on the Xianxian High using drilling data obtained from the southern Raoyang Sag.We discuss here the timing and genetic model of the Xianxian metamorphic core complex based on comprehensive consideration of its developmental characteristics and background in the North China Craton.Our study shows that(1)the curved Xianxian fault in the study area has the characteristics of the main detachment fault;(2)the southern Raoyang Sag,located in the hanging wall of the fault,shows residual Middle Proterozoic to Lower Paleozoic accompanied by numerous secondary faults with different dips in the sag;and(3)the Archean to Paleoproterozoic strata constitute the main part of the Xianxian High with lithology including hornblende,biotite monzonitic and localized granite gneisses.Overall,our results demonstrate that the Xianxian metamorphic core complex,formed in the Late Mesozoic(K1?),has the basic characteristics of a typical metamorphic core complex.It developed in the background of the largescale lithospheric thinning of the eastern North China Craton and evolved in accordance with the rollinghinge model.
引文
[1]DAVIS G A,CONEY P J.Geologic development of the Cordilleran metamorphic core complexes[J].Geology,1979,7:120-124.
[2]CONEY P J,HARMS T A.Cordilleran metamorphic core complexes:Cenozoic extensional relics of Mesozoic compression[J].Geology,1984,12:550-554.
[3]宋鸿林.变质核杂岩研究进展、基本特征及成因探讨[J].地学前缘,1995,2(1):103-111.
[4]吴福元,徐义刚,高山,等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报,2008,24(6):1145-1174.
[5]CHEN L.Concordant structural variations from the surface to the base of the upper mantle in the North China Craton and its tectonic implications[J].Lithos,2010,120:96-115.
[6]朱日祥,陈凌,吴福元,等.华北克拉通破坏的时间、范围与机制[J].中国科学D辑:地球科学,2011,41(5):583-592.
[7]朱日祥,徐义刚,朱光,等.华北克拉通破坏[J].中国科学D辑:地球科学,2012,42(8):1135-1159.
[8]段秋梁,谭未一,杨长春,等.华北东部晚中生代伸展构造作用[J].地球物理学进展,2007,22(2):403-410.
[9]刘俊来,DAVIS G A,纪沫,等.地壳的拆离作用与华北克拉通破坏:晚中生代伸展构造约束[J].地学前缘,2008,15(3):72-81.
[10]林伟,王清晨,王军,等.辽东半岛晚中生代伸展构造:华北克拉通破坏的地壳响应[J].中国科学D辑:地球科学,2011,21(5):638-653.
[11]林伟,王军,刘飞,等.华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论[J].岩石学报,2013,29(5):1791-1810.
[12]王涛,郑亚东,张进江,等.华北克拉通中生代伸展构造研究的几个问题及其在岩石圈减薄研究中的意义[J].地质通报,2007,26(9):1154-1166.
[13]刘俊来,关会梅,纪沫,等.华北晚中生代变质核杂岩构造及其对岩石圈减薄机制的约束[J].自然科学进展,2006,16(1):21-26.
[14]牛树银.太行山阜平、赞皇隆起是中新生代变质核杂岩[J].地质科技情报,1994,13(2):15-16.
[15]牛树银,许传诗,国连杰,等.太行山变质核杂岩的特征及成因探讨[J].河北地质学院学报,1994,17(1):43-53.
[16]马寅生,崔盛芹,吴淦国,等.医巫闾山变质核杂岩构造特征[J].地球学报,1999,20(4):385-391.
[17]王新社,郑亚东,张进江,等.呼和浩特变质核杂岩伸展运动学特征及剪切作用类型[J].地质通报,2002,21(4/5):238-245.
[18]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):411-419.
[19]胡正国,钱壮志.小秦岭西段拆离-变质核杂岩构造[J].地质找矿论丛,1994,9(2):58-66.
[20]高光明,彭恩生,郭宇杰.河南熊耳山北坡西段的变质核杂岩和拆离断层[J].中南矿冶学院学报,1993,24(5):579-584.
[21]姚丽景,颜丹平,胡玲.房山变质核杂岩基底拆离断层韧性剪切变形构造及环境分析[J].地球科学:中国地质大学学报,2007,32(3):357-365.
[22]WANG T,ZHENG Y D,ZHANG J J,et al.Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia:perspectives from metamorphic core complexes[J].Tectonics,2011,30:TC6007.http:∥dx.doi.org/10.1029/2011TC002896.
[23]冀文斌,林伟,石永红,等.大别山早白垩世变质核杂岩的结构与演化[J].地质科学,2011,46(1):161-180.
[24]陈印,朱光,姜大志,等.云蒙山变质核杂岩的变形规律与发育机制[J].科学通报,2014,59(16):1525-1541.
[25]张必龙,朱光,陈印,等.辽西瓦子峪变质核杂岩的变形规律与成因[J].中国科学D辑:地球科学,2013,43(8):1249-1267.
[26]LIN W,FAURE M,CHEN Y,et al.Late Mesozoic compressional to extensional tectonics in the Yiwulvshan massif,NE China and its bearing on the evolution of the YinshanYanshan orogenic belt.PartⅠ:structural analyses and geochronological constraints[J].Gondwana Research,2013,23:54-77.
[27]WANG T,GUO L,ZHENG Y D,et al.Timing and processes of late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton:mainly constrained by zircon U-Pb ages from metamorphic core complexes[J].Lithos,2012,154:315-345.
[28]王巧云,颜丹平,苏本勋,等.京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化[J].地质通报,2006,25(4):448-453.
[29]李三忠,索艳慧,戴黎明,等.渤海湾盆地形成与华北克拉通破坏[J].地学前缘,2010,17(4):64-89.
[30]HE L J,WANG J Y.Cenozoic thermal history of the Bohai Bay Basin:constraints from heat flow and coupled basinmountain modeling[J].Physics and Chemistry of the Earth,2003,28:421-429.
[31]孙冬胜.冀中坳陷中区中新生代复合伸展构造[D].西安:西北大学,2001:1-99.
[32]何登发,崔永谦,张煜颖,等.渤海湾盆地冀中坳陷古潜山的构造成因类型[J].岩石学报,2017,33(4):1338-1356.
[33]ZHAO G C,SUN M,WILDE S A,et al.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J].Precambrian Research,2005,136(2):177-202.
[34]翟明国.华北克拉通的形成演化与成矿作用[J].矿床地质,2010,29(1):24-36.
[35]侯贵廷.渤海湾盆地地球动力学[M].北京:科学出版社,2014:29-112.
[36]翟明国,朱日祥,刘建明,等.华北东部中生代构造体制转折的关键时限[J].中国科学D辑,2003,33(10):913-920.
[37]翟明国,孟庆仁,刘建明,等.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨[J].地学前缘,2004,11(3):285-297.
[38]MAO L G,XIAO A C,ZHANG H W,et al.Structural patterns of the late Mesozoic crustal detachment system in the Raoyang Sag,Bohai Bay Basin,eastern China:new insights from 3Dseismic data[J].Marine and Petroleum Geology,2017,84:215-224.
[39]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):8-22.
[40]ALLEN M B,MACDONALD D I M,ZHAO X,et al.Early Cenozoic two-phase extension and late Cenozoic thermal subsidence and inversion of the Bohai Basin,northern China[J].Marine and Petroleum Geology,1997,14(7):951-972.
[41]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.
[42]漆家福,张一伟,陆克政,等.渤海湾盆地新生代构造演化[J].石油大学学报(自然科学版),1995(增刊):1-6.
[43]何登发,崔永谦,单帅强,等.渤海湾盆地冀中坳陷古潜山的三维地质结构特征[J].地质科学,2018,53(1):1-24.
[44]DAVIS G A,郑亚东.变质核杂岩的定义、类型及构造背景[J].地质通报,2002,21(4/5):185-192.
[45]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面[J].地质学报,1991,65(3):199-215.
[46]刘国栋,史书林,王宝钧.华北地区壳内高导层及其与地壳构造活动性的关系[J].中国科学B辑,1984,14(9):839-848.
[47]孙武城,李松林,罗力雷,等.初论华北地区的地壳低速层[J].地震地质,1987,9(1):17-26.
[48]魏文博,谭捍东,金胜,等.华北中部岩石圈电性结构:应县-商河剖面大地电磁测深研究[J].地球科学:中国地质大学学报,2002,27(5):645-650.
[49]詹艳,赵国泽,王立凤,等.河北石家庄地区深部结构大地电磁探测[J].地震地质,2011,33(4):913-927.
[50]JIA S X,WANG F Y,TIAN X F,et al.Crustal structure and tectonic study of North China Craton from a long deep seismic sounding profile[J].Tectonophysics,2014,627:48-56.
[51]王椿镛,张先康,吴庆举.冀中坳陷内深地震反射剖面揭示的滑脱构造[J].科学通报,1994,39(7):625-628.
[52]王椿镛,张先康,吴庆举,等.华北盆地滑脱构造的地震学证据[J].地球物理学报,1994,37(5):613-620.
[53]王椿镛,张先康,林中洋,等.束鹿断陷盆地及其临近的地壳结构特征[J].地震学报,1994,16(4):472-479.
[54]舒良树,孙岩,王德滋,等.华南武功山中生代伸展构造[J].中国科学D辑,1998,28(5):431-438.
[55]DARBY B J,DAVIS G A,ZHANG X H,et al.辽西医巫闾山地区瓦子峪变质核杂岩的厘定[J].地学前缘,2004,11(3):145-155.
[56]杜旭东,李洪革,陆克政,等.华北地台东部及邻区中生代(J-K)原型盆地分布及成盆模式探讨[J].石油勘探与开发,1999,26(4):5-9.
[57]DAVIS G A,DARBY B J,ZHENG Y D,et al.Geometric and temporal evolution of an extensional detachment fault,Hohhot metamorphic core complex,Inner Mongolia,China[J].Geology,2002,30:1003-1006.
[58]WANG X S,ZHENG Y D,JIA W.Extension of the Louzidian metamorphic core complex and development of supradetachment basins in southern Chifeng,Inner Mongolia,China[J].Acta Geologica Sinica,2004,78:237-245.
[59]孙冬胜,刘池阳,杨明慧,等.渤海湾盆地冀中坳陷中区中新生代复合伸展构造[J].地质论评,2004,50(5):484-491.
[60]杨明慧,刘池阳,杨斌谊,等.冀中坳陷古近纪的伸展构造[J].地质论评,2002,48(1):58-67.
[61]杨明慧,刘池阳,孙冬胜,等.冀中坳陷的伸展构造系统及其构造背景[J].大地构造与成矿学,2002,26(2):113-120.
[62]QI J F,YANG Q.Cenozoic structural deformation and dynamic processes of the Bohai Bay basin province,China[J].Marine and Petroleum Geology,2010,27:757-771.
[2]CONEY P J,HARMS T A.Cordilleran metamorphic core complexes:Cenozoic extensional relics of Mesozoic compression[J].Geology,1984,12:550-554.
[3]宋鸿林.变质核杂岩研究进展、基本特征及成因探讨[J].地学前缘,1995,2(1):103-111.
[4]吴福元,徐义刚,高山,等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报,2008,24(6):1145-1174.
[5]CHEN L.Concordant structural variations from the surface to the base of the upper mantle in the North China Craton and its tectonic implications[J].Lithos,2010,120:96-115.
[6]朱日祥,陈凌,吴福元,等.华北克拉通破坏的时间、范围与机制[J].中国科学D辑:地球科学,2011,41(5):583-592.
[7]朱日祥,徐义刚,朱光,等.华北克拉通破坏[J].中国科学D辑:地球科学,2012,42(8):1135-1159.
[8]段秋梁,谭未一,杨长春,等.华北东部晚中生代伸展构造作用[J].地球物理学进展,2007,22(2):403-410.
[9]刘俊来,DAVIS G A,纪沫,等.地壳的拆离作用与华北克拉通破坏:晚中生代伸展构造约束[J].地学前缘,2008,15(3):72-81.
[10]林伟,王清晨,王军,等.辽东半岛晚中生代伸展构造:华北克拉通破坏的地壳响应[J].中国科学D辑:地球科学,2011,21(5):638-653.
[11]林伟,王军,刘飞,等.华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论[J].岩石学报,2013,29(5):1791-1810.
[12]王涛,郑亚东,张进江,等.华北克拉通中生代伸展构造研究的几个问题及其在岩石圈减薄研究中的意义[J].地质通报,2007,26(9):1154-1166.
[13]刘俊来,关会梅,纪沫,等.华北晚中生代变质核杂岩构造及其对岩石圈减薄机制的约束[J].自然科学进展,2006,16(1):21-26.
[14]牛树银.太行山阜平、赞皇隆起是中新生代变质核杂岩[J].地质科技情报,1994,13(2):15-16.
[15]牛树银,许传诗,国连杰,等.太行山变质核杂岩的特征及成因探讨[J].河北地质学院学报,1994,17(1):43-53.
[16]马寅生,崔盛芹,吴淦国,等.医巫闾山变质核杂岩构造特征[J].地球学报,1999,20(4):385-391.
[17]王新社,郑亚东,张进江,等.呼和浩特变质核杂岩伸展运动学特征及剪切作用类型[J].地质通报,2002,21(4/5):238-245.
[18]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):411-419.
[19]胡正国,钱壮志.小秦岭西段拆离-变质核杂岩构造[J].地质找矿论丛,1994,9(2):58-66.
[20]高光明,彭恩生,郭宇杰.河南熊耳山北坡西段的变质核杂岩和拆离断层[J].中南矿冶学院学报,1993,24(5):579-584.
[21]姚丽景,颜丹平,胡玲.房山变质核杂岩基底拆离断层韧性剪切变形构造及环境分析[J].地球科学:中国地质大学学报,2007,32(3):357-365.
[22]WANG T,ZHENG Y D,ZHANG J J,et al.Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia:perspectives from metamorphic core complexes[J].Tectonics,2011,30:TC6007.http:∥dx.doi.org/10.1029/2011TC002896.
[23]冀文斌,林伟,石永红,等.大别山早白垩世变质核杂岩的结构与演化[J].地质科学,2011,46(1):161-180.
[24]陈印,朱光,姜大志,等.云蒙山变质核杂岩的变形规律与发育机制[J].科学通报,2014,59(16):1525-1541.
[25]张必龙,朱光,陈印,等.辽西瓦子峪变质核杂岩的变形规律与成因[J].中国科学D辑:地球科学,2013,43(8):1249-1267.
[26]LIN W,FAURE M,CHEN Y,et al.Late Mesozoic compressional to extensional tectonics in the Yiwulvshan massif,NE China and its bearing on the evolution of the YinshanYanshan orogenic belt.PartⅠ:structural analyses and geochronological constraints[J].Gondwana Research,2013,23:54-77.
[27]WANG T,GUO L,ZHENG Y D,et al.Timing and processes of late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton:mainly constrained by zircon U-Pb ages from metamorphic core complexes[J].Lithos,2012,154:315-345.
[28]王巧云,颜丹平,苏本勋,等.京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化[J].地质通报,2006,25(4):448-453.
[29]李三忠,索艳慧,戴黎明,等.渤海湾盆地形成与华北克拉通破坏[J].地学前缘,2010,17(4):64-89.
[30]HE L J,WANG J Y.Cenozoic thermal history of the Bohai Bay Basin:constraints from heat flow and coupled basinmountain modeling[J].Physics and Chemistry of the Earth,2003,28:421-429.
[31]孙冬胜.冀中坳陷中区中新生代复合伸展构造[D].西安:西北大学,2001:1-99.
[32]何登发,崔永谦,张煜颖,等.渤海湾盆地冀中坳陷古潜山的构造成因类型[J].岩石学报,2017,33(4):1338-1356.
[33]ZHAO G C,SUN M,WILDE S A,et al.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J].Precambrian Research,2005,136(2):177-202.
[34]翟明国.华北克拉通的形成演化与成矿作用[J].矿床地质,2010,29(1):24-36.
[35]侯贵廷.渤海湾盆地地球动力学[M].北京:科学出版社,2014:29-112.
[36]翟明国,朱日祥,刘建明,等.华北东部中生代构造体制转折的关键时限[J].中国科学D辑,2003,33(10):913-920.
[37]翟明国,孟庆仁,刘建明,等.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨[J].地学前缘,2004,11(3):285-297.
[38]MAO L G,XIAO A C,ZHANG H W,et al.Structural patterns of the late Mesozoic crustal detachment system in the Raoyang Sag,Bohai Bay Basin,eastern China:new insights from 3Dseismic data[J].Marine and Petroleum Geology,2017,84:215-224.
[39]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):8-22.
[40]ALLEN M B,MACDONALD D I M,ZHAO X,et al.Early Cenozoic two-phase extension and late Cenozoic thermal subsidence and inversion of the Bohai Basin,northern China[J].Marine and Petroleum Geology,1997,14(7):951-972.
[41]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.
[42]漆家福,张一伟,陆克政,等.渤海湾盆地新生代构造演化[J].石油大学学报(自然科学版),1995(增刊):1-6.
[43]何登发,崔永谦,单帅强,等.渤海湾盆地冀中坳陷古潜山的三维地质结构特征[J].地质科学,2018,53(1):1-24.
[44]DAVIS G A,郑亚东.变质核杂岩的定义、类型及构造背景[J].地质通报,2002,21(4/5):185-192.
[45]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面[J].地质学报,1991,65(3):199-215.
[46]刘国栋,史书林,王宝钧.华北地区壳内高导层及其与地壳构造活动性的关系[J].中国科学B辑,1984,14(9):839-848.
[47]孙武城,李松林,罗力雷,等.初论华北地区的地壳低速层[J].地震地质,1987,9(1):17-26.
[48]魏文博,谭捍东,金胜,等.华北中部岩石圈电性结构:应县-商河剖面大地电磁测深研究[J].地球科学:中国地质大学学报,2002,27(5):645-650.
[49]詹艳,赵国泽,王立凤,等.河北石家庄地区深部结构大地电磁探测[J].地震地质,2011,33(4):913-927.
[50]JIA S X,WANG F Y,TIAN X F,et al.Crustal structure and tectonic study of North China Craton from a long deep seismic sounding profile[J].Tectonophysics,2014,627:48-56.
[51]王椿镛,张先康,吴庆举.冀中坳陷内深地震反射剖面揭示的滑脱构造[J].科学通报,1994,39(7):625-628.
[52]王椿镛,张先康,吴庆举,等.华北盆地滑脱构造的地震学证据[J].地球物理学报,1994,37(5):613-620.
[53]王椿镛,张先康,林中洋,等.束鹿断陷盆地及其临近的地壳结构特征[J].地震学报,1994,16(4):472-479.
[54]舒良树,孙岩,王德滋,等.华南武功山中生代伸展构造[J].中国科学D辑,1998,28(5):431-438.
[55]DARBY B J,DAVIS G A,ZHANG X H,et al.辽西医巫闾山地区瓦子峪变质核杂岩的厘定[J].地学前缘,2004,11(3):145-155.
[56]杜旭东,李洪革,陆克政,等.华北地台东部及邻区中生代(J-K)原型盆地分布及成盆模式探讨[J].石油勘探与开发,1999,26(4):5-9.
[57]DAVIS G A,DARBY B J,ZHENG Y D,et al.Geometric and temporal evolution of an extensional detachment fault,Hohhot metamorphic core complex,Inner Mongolia,China[J].Geology,2002,30:1003-1006.
[58]WANG X S,ZHENG Y D,JIA W.Extension of the Louzidian metamorphic core complex and development of supradetachment basins in southern Chifeng,Inner Mongolia,China[J].Acta Geologica Sinica,2004,78:237-245.
[59]孙冬胜,刘池阳,杨明慧,等.渤海湾盆地冀中坳陷中区中新生代复合伸展构造[J].地质论评,2004,50(5):484-491.
[60]杨明慧,刘池阳,杨斌谊,等.冀中坳陷古近纪的伸展构造[J].地质论评,2002,48(1):58-67.
[61]杨明慧,刘池阳,孙冬胜,等.冀中坳陷的伸展构造系统及其构造背景[J].大地构造与成矿学,2002,26(2):113-120.
[62]QI J F,YANG Q.Cenozoic structural deformation and dynamic processes of the Bohai Bay basin province,China[J].Marine and Petroleum Geology,2010,27:757-771.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |