Study on the formation and evolution of deep structure of Xujiaweizi fault depression
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摘要: 徐家围子断陷是松辽盆地北部深层最重要的含气断陷。本文根据最新地震和钻井资料综合研究成果,结合前人研究认识,探讨了徐家围子断陷的形成与演化,认为徐家围子断陷在区域构造位置上处于东北地区松辽盆地的北部,处于松辽盆地区域莫霍面隆起的西斜坡上,特定的位置决定了其形成演化的各个阶段受东北地区区域板块构造运动的控制,与松辽盆地的形成与演化具有一定的关系。徐家围子断陷形成与演化可以划分为5个阶段,是太平洋构造域板块间的相互作用和深部热力作用发育演化的结果,这种过程造就了现今南北分块、东西分带、凹隆相间、构造复杂和沉积岩与火山岩并存的地质结构。徐家围子断陷深层现今构造格局受控于近NW向的徐中断裂、近SN向的徐西断裂、近NW向的徐东断裂带和四组近NE向的断裂。本次研究,对以往无法解释的很多地质现象给予了很好的解释,得出了一些崭新的认识,也从宏观上为寻找天然气资源给予了有力指导。Abstract: Xujiaweizi fault depression is the most important gas-bearing fault depression in the deep of Songliao basin. On the basis of the latest seismic and drilling data research achievements, this article research the formation and evolution of Xujiaweizi fault depression again, combining with the recognition of predecessors. Xujiaweizi fault depression is situated in the north of Songliao basin, and on the western slope of Moho uplift in regional tectonic position, the specific position of Xujiaweizi fault depression has decided that its every stage of formation and evolution is controlled by the tectonic movement of northern regional plate. It also has certain relationship with formation and evolution of Songliao basin. We can divide the formation and evolution of Xujiaweizi fault depression into five stages, which is the result of development and formation course of interaction of Pacific tectonic plates and action of deep thermal. This periodic cycles of processing has created the present geological structure with the characteristic, which is different segmentation from south to north, various zones from east to west, alternating with protruding and sunken belt,structurally complex and sedimentary coexist with volcanic rocks. Xujiaweizi fault depression deep zones are controlled by four sets of faults, such as nearly north-west Xuzhong fault, nearly south-north Xuxi fault, nearly north-west Xudong fault belt and four groups of nearly north-east fault. This research offers well interpretations for a lot of the past geological phenomena we can't explain, and obtains some new recognition, which gives effective guidance to find natural gas resource from macro-level at the same time.
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[1] Chi YL,Yun JB,Meng QA,Deep Structure and Dynamic of the Songliao Basin for Hydrocarbon Accumulation,北京:石油工业出版社,2002.
[2] Condie KC,Mantle Plumes and Their Record in Earth History,London:cambridge University Press,2001.
[3] Engebretson DC,Cox A,Gordon RG,Relative motions between oceanic and continental plates in the Pacific basin,The Geological Society of America (Special Paper),1985.
[4] Gao J,Li ZL,Li QX,Crustal structure beneath northern Songliao Basin and Songliao Basin genesis mechanism,Petroleum Geology & Oilfield Development in Daqing,2002(1).
[5] Gao RQ,Cai XY,Formation Conditions and Distribution Regularities of Oil & Gas Field in Songliao Basin,北京:石油工业出版社,1997.
[6] Hu WS,Structural charactefistics and petroleum system in rift-type Songlian Basin in Mesozoic and Cenozoic,Journal of Jianghan Petroleum Institute,1997(1).
[7] Li J,Shu LS,Mesozoic-Cenozoic tectonic features and evolution of the Songliao Basin,NE China,Journal of Nanjing University(Natural Science),2002(4).
[8] Li ST,Basin geodynamics background of formation of huge petroleum systems,Earth Science-Journal of China University of Geoscieaces,2004(5).
[9] Li ZA,Yin ZM,Simulation study of dynamic force mechanism for evolution of Songliao Basin structure China,Petroleum Exploration,1999(4).
[10] Liu DI,Chen FJ,Tang JR,Formation,development of Songliao Basin and dynamics of lithosphere,Chinese Journal of Geology(Scientia Geologica Sinica),1996(4).
[11] Liu DL,Ma L,Mesozoic tectonic evolution of continental margin in east Asia,Geoscience,1997(4).
[12] Liu DL,Ma L,Relation between prerift volcanic and the rift basin and geodynamic processes,Geological Review,1998(2).
[13] Liu XF,Zhong GF,Wang ZY,Chen Q,Tectonic framework of Xujiaweizi fault depression in northern Scngliao Basin and its origin,Journal of Xi\'an Petroleum University(Natural Science Edition),2006(4).
[14] Luo Q,Sun HZ,Discordogenic faults and their controlling action on natural in Songliao Basin,Natural Gas Industry,2000(3).
[15] Ma L,Liu DL,The origin and evolution of Songliao Basin and its relation with asthenosphere convection mode,Chinese Journal of Geology(Scientia Geologiea Sinica),1999(3).
[16] Maruyama S,lsozaki Y,Kimura G,Paleogeographic maps of the Japanese islands:Plate tectonic synthesis from 750Ma to the present,Island Arc,1997(1).
[17] Pirajno F,Ore Deposits and Mineral Deposits,Dordrecht,the Netherlands:Kluwer Academic Publishers,2000.
[18] 任延广.朱德丰.万传彪.冯子辉.李景坤.王成 松辽盆地徐家围子断陷天然气聚集规律与下步勘探方向 [J].-大庆石油地质与开发2004(5)
[19] Ren SM,Huang BC,Preliminary study on post-late Paleozoic kinematics of the main blocks of the Palee-Asian Ocean,Progress In Geophysics,2002(1).
[20] Shao JA,Zhao GL,Wang Z,Tectonic setting of Mesozoic volcanic activity in Daxinganling,Geological Review,1999(zk).
[21] Song JQ,Plate movement on the impact of Songliao basin\'s tectonic evolution,Science and Technology Consulting Herald,2008.
[22] Sun WD,Ling MX,Wang FY,Pacific plate subduction and Mesozoic geological event in eastern China,Bulletin of Mineralogy Petrology and Geochemistry,2008(3).
[23] Sun XM,Wang PJ,Hao FJ,Space-time distribution features,migration regularities and genetic types of regional fault system of Mesozoic-Cenozoic in the central section of epicontinent of the east Chino,Journal of Jilin University(Earth Science Edition),2005(5).
[24] Sun XM,Long SX,Zhang MS,Discovery and timing of major thrustbelt in Jiamnsi-Yitong fault zone,Oil & Gas Geology,2006(5).
[25] Wilson JT,A possible origin of the Hawaiian islands,Canadian Journal of Physics,1963.
[26] Xiao L,Wang FZ,Wang H,Mantle plume tectonics constraints on the formation of Songliac and Bohaiwan Basins,Earth Sciences,2004(3).
[27] Yang BJ,Tang JR,Li QX,The crust reflection structure in uplift area of Songliac Basin and disconnected Mo-Huo interlace,Science in China,2003(2).
[28] 殷进垠.刘和甫.迟海江 松辽盆地徐家围子断陷构造演化 [J].-石油学报2002(2)
[29] Yu HZ,Li YW,Han SH,Tectonic evolution of Songliao basin in the Palaeozoic,Geotectonica Et Metallogenia,2001(4).
[30] 云金表.金之钧.殷进垠.赵利华.庞庆山 松辽盆地徐家围子地区深反射结构及其盆地动力学意义 [J].-地学前缘2008(4)
[31] Zhao Y,Yang ZY,Ma XH,Tectonic development of the important turning point in East Asian,Chinese Journal of Geology(Scientia Geologica Sinica),1994(2).
[32] Zhang QL,Wang LS,Xie GA,Discussion on northward extension of the Tanlu fault zone and its tectonic regime transformation,Geological Journal of China Universities,2005(4).
[33] Zhang YG,Chen SM,Zhang EH,The new progress of Xujiaweizi fault depression characteristics of structural geology research,Acta Pctrologica Sinics,2010(1).
[34] Zhu G,Niu ML,Liu GS,Structural,magmatic and sedimentary events of the Tan-Lu fault belt during its Early Cretaceous strike-slip movement,Acta Geologica Sinica,2002(3).
[35] Zhu G,Liu GS,Niu ML,Transcurrent movement and genesis of the Tan-Lu fault zone,Regional Geology of China,2003(3).
[36] 迟元林,云金表,蒙启安,松辽盆地深部结构及盆地动力学与油气聚集,北京:石油工业出版社,2002.
[37] 高君.李占林.李勤学 松辽盆地北部深部地壳结构及盆地成因机制 [J].-大庆石油地质与开发2002(1)
[38] 高瑞棋,蔡希源,松辽盆地油气田形成条件与分布规律,北京:石油工业出版社,1997.
[39] 胡望水 松辽裂谷型盆地构造特征与含油气系统 [J].-石油天然气学报1997(1)
[40] 李娟.舒良树 松辽盆地中、新生代构造特征及其演化 [J].-南京大学学报(自然科学版)2002(4)
[41] 李思田 大型油气系统形成的盆地动力学背景 [J].-地球科学-中国地质大学学报2004(5)
[42] 李自安,尹中民,松辽盆地构造演化力源机制的模拟研究,中国石油勘探,1999(4).
[43] 刘德来,陈发景,唐建人,松辽盆地形成、发展与岩石圈动力学,地质科学,1996(4).
[44] 刘德来.马莉 中生代东亚大陆边缘构造演化 [J].-现代地质1997(4)
[45] 刘德来.马莉 松辽盆地裂谷期前火山岩与裂谷盆地关系及动力学过程 [J].-地质论评1998(2)
[46] 刘学锋.钟广法.王正允.陈强 松辽盆地北部徐家围子断陷构造格局及其成因 [J].-西安石油大学学报（自然科学版）2006(4)
[47] 罗群.孙宏智 松辽盆地深大断裂对天然气的控制作用 [J].-天然气工业2000(3)
[48] 马莉,刘德来,松辽盆地成因演化与软流圈对流模式,地质科学,1999(3).
[49] 任延广.朱德丰.万传彪.冯子辉.李景坤.王成 松辽盆地徐家围子断陷天然气聚集规律与下步勘探方向 [J].-大庆石油地质与开发2004(5)
[50] 任收麦.黄宝春 晚古生代以来古亚洲洋构造域主要块体运动学特征初探 [J].-地球物理学进展2002(1)
[51] 邵济安.赵国龙.王忠.韩庆军 兴安岭中生代火山活动构造背景 [J].-地质论评1999(z1)
[52] 宋均秋 板块运动对松辽盆地构造演化的影响 [J].-科技创新导报2008(30)
[53] 孙卫东.凌明星.汪方跃.丁兴.胡艳华.周继彬.杨晓勇 太平洋板块俯冲与中国东部中生代地质事件 [J].-矿物岩石地球化学通报2008(3)
[54] 孙晓猛.王璞珺.郝福江.包亚范.马旭.韩国卿 中国东部陆缘中区中-新生代区域断裂系统时空分布特征、迁移规律及成因类型 [J].-吉林大学学报（地球科学版）2005(5)
[55] 孙晓猛.龙胜祥.张梅生.刘晓燕.郝福江 佳木斯-伊通断裂带大型逆冲构造带的发现及形成时代 [J].-石油与天然气地质2006(5)
[56] 肖龙.王方正.王华.F.Pirajno 地幔柱构造对松辽盆地及渤海湾盆地形成的制约 [J].-地球科学-中国地质大学学报2004(3)
[57] 杨宝俊,唐建人,李勤学,松辽盆地隆起区地壳反射结构与"断开"莫霍界面,中国科学A辑,2003(2).
[58] 殷进垠.刘和甫.迟海江 松辽盆地徐家围子断陷构造演化 [J].-石油学报2002(2)
[59] 余和中.李玉文.韩守华.易万霞 松辽盆地古生代构造演化 [J].-大地构造与成矿学2001(4)
[60] 云金表.金之钧.殷进垠.赵利华.庞庆山 松辽盆地徐家围子地区深反射结构及其盆地动力学意义 [J].-地学前缘2008(4)
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