新生代郯庐断裂活动在莱州湾地区的响应
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摘要
运用最新的三维地震资料,对渤海南部海域郯庐断裂的空间展布特征进行了刻画,综合分析了郯庐断裂在研究区内活动演化史及其对该区域内沉积和圈闭的影响。郯庐断裂在研究区渤海南部海域内表现出了明显的花状构造和地层拖曳现象,东支断裂南部的盐构造南北向展布也证实了郯庐断裂新生代以来确实发生过走滑活动;郯庐断裂的活动演化对莱州湾凹陷产生了重要影响,主要体现在渐新世的走滑活动导致了莱州湾凹陷沉积中心向凹陷东北方向发生了偏移,并在深浅层形成了以断背斜、半背斜和断块为主的圈闭。
By using the latest 3D seismic data,we described the space distribution of the Tan-Lu fault in the southern Bohai area and analyzed the evolution history and the influence to sedimentation and tarp formation combining the previous research achievements.The results showed that: in the southern Bohai area,flower structure and formation dag were revealed in the Tan-Lu fault and the salt activity was also a strong evidence for the strik-slip movement of the Tan-Lu fault in Cenozoic.The activity of the Tan-Lu fault had a significant impact on the evolution of the Laizhou Bay Sag,mainly reflected by the migration of sedimentary center.It also led to the formation of traps in both deep and shallow layers and most of the traps were faulted anticlines and fault blocks.
By using the latest 3D seismic data,we described the space distribution of the Tan-Lu fault in the southern Bohai area and analyzed the evolution history and the influence to sedimentation and tarp formation combining the previous research achievements.The results showed that: in the southern Bohai area,flower structure and formation dag were revealed in the Tan-Lu fault and the salt activity was also a strong evidence for the strik-slip movement of the Tan-Lu fault in Cenozoic.The activity of the Tan-Lu fault had a significant impact on the evolution of the Laizhou Bay Sag,mainly reflected by the migration of sedimentary center.It also led to the formation of traps in both deep and shallow layers and most of the traps were faulted anticlines and fault blocks.
引文
[1]张鹏,王良书,石火生,等.郯庐断裂带山东段的中新生代构造演化特征[J].地质学报,2010,84(9):1316-1323.
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[3]朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学,2004,39(1):36-49.
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[5]万天丰,朱鸿,赵磊,等.郯庐断裂带的形成与演化:综述[J].现代地质,1996,10(2):159-168.
[6]朱光,王勇生,牛漫兰,等.郯庐断裂带的同造山运动[J].地学前缘,2004,11(3):169-182.
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[9]吴根耀,马力,梁兴,等.从郯庐断裂带两侧的“盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008,27(3):308-325.
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[12]万天丰.中国中、新生代板内变形与构造应力场[J].地质力学学报,1996,2(3):13.
[13]张岳桥,董树文.郯庐断裂带中生代构造演化史:进展与新认识[J].地质通报,2008,27(9):1371-1390.
[14]朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003,22(3):200-207.
[15]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995,10(2):121-134.
[16]肖文交,周烑秀,杨振宇,等.大别—郯庐—苏鲁造山带复合旋转拼贴作用[J].地球科学进展,2000,15(2):147-153.
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[18]Yin A,Nie S Y.An indendation model for the North and South Chinacollision and the development of the Tan-Lu and Honam faultsystem,eastern Asia[J].Tectonics,1993,12(4):801-803.
[19]Chang E Z.Collision orogene between north and south Chinaand its eastern extension in the Korean Peninsula[J].Journalof Southeast Asian Earth Science,1996,13(3):267-277.
[20]宗国洪.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282.
[21]汤良杰,陈绪云,周心怀,等.渤海海域郯庐断裂带构造解析[J].西南石油大学学报:自然科学版,2011,33(1):170-176.
[22]王亮,牛成民,杨波,等.莱州湾凹陷沙三段含油气系统与有利勘探方向[J].断块油气田,2011,18(5):545-548.
[23]牛成民.渤海南部海域莱州湾凹陷构造演化与油气成藏[J].石油与天然气地质,2012,33(3):424-431.
[24]杨波,曾选萍,王改卫,等.莱州湾凹陷油气成藏主控因素分析[J].重庆科技学院学报:自然科学版,2011,13(1):6-9.
[25]彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30(5):654-660.
[26]Yu Yixin,Zhou Xinhuai,Tang Liangjie,et al.Salt structures inthe Laizhouwan depression,offshore Bohai Bay basin,easternChina:New insights from 3D seismic data[J].Marine and Pe-troleum Geology,2009,26(8):1600-1607.
[27]余一欣,周心怀,徐长贵,等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质,2011,32(2):273-279.
[28]江涛,邱玉超,邓校国,等.狭长走滑断陷盆地构造对沉积—成藏的控制作用:以伊通盆地为例[J].石油实验地质,2012,34(3):267-271.
[29]王永利,武强,王应斌.莱州湾凹陷西走滑带构造演化特征及对油气成藏的影响[J].石油地质与工程,2010,24(2):5-8.
[30]邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气地质,2001,15(5):2-6.
[31]马庆佑,沙旭光,李玉兰,等.塔中顺托果勒区块走滑断裂特征及控油作用[J].石油实验地质,2012,34(2):120-124.
[2]许志琴.郯庐裂谷系概述[J].构造地质论丛,1984(3):39-46.
[3]朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学,2004,39(1):36-49.
[4]陈宣华,王小凤,张青,等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000,30(3):215-220.
[5]万天丰,朱鸿,赵磊,等.郯庐断裂带的形成与演化:综述[J].现代地质,1996,10(2):159-168.
[6]朱光,王勇生,牛漫兰,等.郯庐断裂带的同造山运动[J].地学前缘,2004,11(3):169-182.
[7]程捷,万天丰.郯庐断裂带在新生代的演化[J].地质科技情报,1996,15(3):36-43.
[8]乔秀夫,张安棣.华北块体、胶辽朝块体与郯庐断裂[J].中国地质,2002,29(4):337-345.
[9]吴根耀,马力,梁兴,等.从郯庐断裂带两侧的“盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008,27(3):308-325.
[10]吴根耀,梁兴,陈焕疆.试论郯城—庐江断裂带的形成、演化及其性质[J].地质科学,2007,42(1):160-175.
[11]徐嘉炜,崔可锐,朱光,等.中国东部郯—庐断裂系统平移研究的若干进展[J].合肥工业大学学报,1984,1(2):28-37.
[12]万天丰.中国中、新生代板内变形与构造应力场[J].地质力学学报,1996,2(3):13.
[13]张岳桥,董树文.郯庐断裂带中生代构造演化史:进展与新认识[J].地质通报,2008,27(9):1371-1390.
[14]朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003,22(3):200-207.
[15]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995,10(2):121-134.
[16]肖文交,周烑秀,杨振宇,等.大别—郯庐—苏鲁造山带复合旋转拼贴作用[J].地球科学进展,2000,15(2):147-153.
[17]Gilder S A,Leloup P H.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via middle Triassic to Early Cenozoicpaleomagnetic data[J].Journal of Geophysical Research,1999,104(7):15365-15390.
[18]Yin A,Nie S Y.An indendation model for the North and South Chinacollision and the development of the Tan-Lu and Honam faultsystem,eastern Asia[J].Tectonics,1993,12(4):801-803.
[19]Chang E Z.Collision orogene between north and south Chinaand its eastern extension in the Korean Peninsula[J].Journalof Southeast Asian Earth Science,1996,13(3):267-277.
[20]宗国洪.济阳坳陷构造演化及其大地构造意义[J].高校地质学报,1999,5(3):275-282.
[21]汤良杰,陈绪云,周心怀,等.渤海海域郯庐断裂带构造解析[J].西南石油大学学报:自然科学版,2011,33(1):170-176.
[22]王亮,牛成民,杨波,等.莱州湾凹陷沙三段含油气系统与有利勘探方向[J].断块油气田,2011,18(5):545-548.
[23]牛成民.渤海南部海域莱州湾凹陷构造演化与油气成藏[J].石油与天然气地质,2012,33(3):424-431.
[24]杨波,曾选萍,王改卫,等.莱州湾凹陷油气成藏主控因素分析[J].重庆科技学院学报:自然科学版,2011,13(1):6-9.
[25]彭文绪,辛仁臣,孙和风,等.渤海海域莱州湾凹陷的形成和演化[J].石油学报,2009,30(5):654-660.
[26]Yu Yixin,Zhou Xinhuai,Tang Liangjie,et al.Salt structures inthe Laizhouwan depression,offshore Bohai Bay basin,easternChina:New insights from 3D seismic data[J].Marine and Pe-troleum Geology,2009,26(8):1600-1607.
[27]余一欣,周心怀,徐长贵,等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质,2011,32(2):273-279.
[28]江涛,邱玉超,邓校国,等.狭长走滑断陷盆地构造对沉积—成藏的控制作用:以伊通盆地为例[J].石油实验地质,2012,34(3):267-271.
[29]王永利,武强,王应斌.莱州湾凹陷西走滑带构造演化特征及对油气成藏的影响[J].石油地质与工程,2010,24(2):5-8.
[30]邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气地质,2001,15(5):2-6.
[31]马庆佑,沙旭光,李玉兰,等.塔中顺托果勒区块走滑断裂特征及控油作用[J].石油实验地质,2012,34(2):120-124.
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