天然气地球科学

• 天然气地质学 • 上一篇    下一篇

巴兰三角洲地区构造特征及其成藏控制因素

马良涛,王居峰,牛嘉玉,郑求根   

  1. 1.中国石油勘探开发研究院,北京 100083;
    2.中国地质大学(北京)海洋学院,北京 100083
  • 收稿日期:2013-12-18 修回日期:2014-03-21 出版日期:2014-06-10 发布日期:2014-06-10
  • 通讯作者: 马良涛maliangtao123@163.com E-mail:maliangtao123@163.com
  • 作者简介:马良涛(1984-),男,四川遂宁人,博士研究生,主要从事石油天然气地质综合研究、层序和沉积分析研究. E-mail:maliangtao123@163.com.
  • 基金资助:

    国家重大专项30-1课题(编号:2008ZX05030-001-04)资助.

Tectonic Characteristics and Hydrocarbon Accumulation Controlling Factors in the Baram Delta Province

MA Liang-tao,WANG Ju-feng,NIU Jia-yu,ZHENG Qiu-gen
  

  1. 1.Research Institute of Petroleum Exploration and Development,Beijing 100083,China;
    2.College of Ocean Science,China University of Geosciences (Beijing),Beijing 100083,China
  • Received:2013-12-18 Revised:2014-03-21 Online:2014-06-10 Published:2014-06-10

摘要:

巴兰三角洲地区位于西北婆罗洲活动大陆边缘,其构造格局具有南北分带的特征,即北部挤压应力下叠瓦状逆冲推覆带、中部拉张应力下伸展沉降带、南部压扭作用下挤压反转带。与位于被动大陆边缘三角洲发育的地区不同,其北部三角洲前端收缩量大于中部三角洲末端伸展量的1.8%左右,而这无法用理想的被动大陆边缘三角洲体模型来进行解释。在研究区区域构造背景、应力特征分析的基础上,认为这种现象是区域压应力远距离效应与三角洲发育过程重力驱动综合作用的结果。受构造南北分带的影响,研究区发育的上部、中部和下部油气成藏组合分布于不同构造带内;各构造带不同应力背景形成了各自内部独特的构造圈闭类型,而作为油气运移通道的长期继承性发育的断层则控制了研究区内油气的垂向运移。这些研究结果对巴兰三角洲地区油气地质研究、油气勘探部署及优选有利勘探新领域具有一定的借鉴和指导意义。

关键词: 巴兰三角洲, 构造特征及成因机制, 油气成藏组合, 成藏控制因素

Abstract:

Baram Delta Province is located at the NW Borneo active margin.It has the features of different zones in north and south: the overlap-thrusting belt under compression in north,extensive subsiding belt generated by extension in middle and compressive inverting belt in south.Different fromthe area developing Cenozoic deltas located on the passive-margin,its total shortening in compression province goes beyond 1.8% compared with the stretching in extension province and this can not be explained by the ideal delta system.Based on the regional tectonic setting analysis and stress features in the study area,it regards the far-field compression and the function driven by gravity during delta growing process as the mechanism for this phenomenon.For the effection of tetonic division,the upper,middle and lower oil-gas reservoir-forming assemblages distributed in different tectonic zone; different stress background generated unique structural trap in various tectonic belt and the fault with long-term activity provided major pathways for hydrocarbon migration.Thus,the conclusion will be helpful for the research of hydrocarbon formation and further hydrocarbon exploration in Baram Delta area.

Key words: Baram Delta Province, Tectonic characteristic and forming mecheanism, Oil-gas reservoir-forming assemblage, Control factors for hydrocarbon accumulation

中图分类号: 

  • TE121

[1]Rosalind C K.Guillaume B,Christopher K M,et al.Balancing deformation in NW Borneo:Quantifying plate-scale vs.gravitational tectonics in a delta and deepwater fold-thrust belt system[J].Marine and Petroleum Geology,2010,27(1):238-246.
[2]Tingay M R P,Hillis R R,Morley C K,et al.Present-day stress orientation in Brunei:A snapshot of ‘prograding tectonics’ in a Tertiary delta[J].Journal of the Geological Society,London ,2005,162(1):39-49.
[3]Tingay M R P,Hillis R R,Morley C K,et al.Variation in vertical stress in the Baram Basin,Brunei:Tectonic and geomechanical implications[J].Marine and Petroleum Geology,2003,20(10):1201-1212.
[4]Zhang Gongcheng,Mi Lijun,Qu Hongjun,et al.Petroleum geology of deep-water areas in offshore China[J].Acta Petrolei Sinica,2013,(supplement2):1-14.[张功成,米立军,屈红军,等.中国海域深水区油气地质[J].石油学报,2013,(supplement2):1-14.]
[5]Zhang Gongcheng,Xie Xiaojun,Wang Wanyin,et al.Tectonic types of petroliferous bsains and its exploration potentian in the South China Sea[J].Acta Petrolei Sinica,2013,34(4):611-627.[张功成,谢晓军,王万银,等.中国南海含油气盆地构造类型及勘探潜力[J].石油学报,2013,34(4):611-627.] 
[6]John H D.Sedimentology and reservoir geology of the Betty field,Baram Delta Province,offshore Sarawak [J].Liang Shirong,translation.Marine Geology,1992(1):85-107.[John H D.婆罗洲西北部沙捞越近海巴兰三角洲地区Betty油田的沉积学和油层地质学特征[J].梁世容译.海洋地质,1992(1):85-107.]
[7]Johnson H D,Kuud T,Dundang A.Sedimentology and reservoir geology of the Betty Field,Baram Delta Province,offshore Sarawak[J].Geology Society Malaysia Bulletin,1989,25:119-161.
[8]Joseph J L.Facies distribution and sedimenttary processes on the modern Baram Delta:Implications for the reservoir sandstones of NW Borneo[J].Zhang Wenlin,Shen Renye,translation.Natural Gas Exploration and Development,2003,26(3):55-64.[Joseph J L.现代巴拉姆三角洲沉积相展布及沉积作用:婆罗洲北西储集砂体研究[J].张闻林,沈人烨译.天然气勘探与开发,2003,26(3):55-64.]
[9]Joseph J L,Abdul A,Abdul R,et al.Facies distribution and sedimentary processes on the modern Baram Delta:Implications for the reservoir sandstones of NW Borneo[J].Marine and Petroleum Geology,2002,19:69-78.
[10]Chen Guomin,Xia Minquan,Wan Yun,et al.Structural characteristics and exploration prospects of north-Kunlun Faults Zone in Qaidam Basin[J].Natural Gas Geoscience,2011,22(1):89-96.[陈国民,夏敏全,万云,等.柴达木盆地昆北断阶带构造特征及油气前景初步评价[J].天然气地球科学,2011,22(1):89-96.]
[11]Rosalind C K,Richard R H,Mark R P,et al.Present-day stress and neotectonic provinces of the Baram Delta and deep-water fold-thrust belt[J].Journal of the Geological Society,London,2009,166:197-200.
[12]Mark R P,Richard R H,Chris K M.Present-day stress and neotectonics of Brunei:Implications for petroleum exploration and production[J].AAPG Bulletin,2009,93:75-100.
[13]King R C,Hillis R R,Tingay R R,et al.Present-day stresses in Brunei,NW Borneo:Superposition of deltaic and active margin tectonics[J].Basin Research,2010,22:236-247.
[14]Hiscott R N.Depositional sequences controlled by high rates of sediment supply,sea-level variations,and growth faulting-the Quaternary Baram Delta of northwestern Borneo[J].Marine Geology,2001,175:67-102.
[15]Mark R P,Birgit M,John R,et al.Understanding tectonic stress in the oil patch:The world stress map project[J].The Leading Edge,2005,24:1276-1282.
[16]Rouby D,Nalpas T,Jermannaud P,et al.Gravity driven deformation controlled by the migration of the delta front:The Plio-Pleistocene of the Eastern Niger Delta[J].Tectonophysics,2011,513:54-67.
[17]Dieter F,Udo B,Ingo H,et al.Seismic images of a collision zone offshore NW Sabah/Borneo[J].Marine and Petroleum Geology,2008,25:606-624.
[18]Zhu Weilin,Hu Ping,Jiang Wenrong,et al.Petroliferous Basins in South Asia and Southeast Asia[M].Beijing:Science Press,2012:223-252.[朱伟林,胡平,江文荣,等.南亚—东南亚含油气盆地[M].北京:科学出版社,2012:223-252.]
[19]Tong Xiaoguang.The meaning of the oil-gas reservoir-forming assemblage in the exploration and evaluation[J].Journal of Southwesst Petroleum Institute,2009,31(6):1-8.[童晓光.论成藏组合在勘探评价中的意义[J].西南石油大学学报,2009,31(6):1-8.]
[20]Xue Liangqing,Yang Fuzhong,Ma Haizhen,et al.Temporal and spatial distribution of tectonic subsidence and discussion on formation mechanism of anomalous post-rift[J].Petroleum Exploration and Development,2005,32(3):130-134.[薛良清,杨福忠,马海珍,等.南苏门达腊盆地中国石油合同区块成藏组合分析[J].石油勘探与开发,2005,32(3):130-134.]
[21]Zhang Zhen,Li Haowu,Duan Hongzhen,et al.Geological characteristics and hydrocarbon accumulation model of the Cenozoic Asmari-Gachsran play,Zagros Basin[J].Oil & Gas Geology,2012,33(2):190-199.[张震,李浩武,段宏臻,等.扎格罗斯盆地新生界Asmari-Gachsaran成藏组合地质特征及成藏模式[J].石油与天然气地质,2012,33(2):190-199.]
[22]Zhou Changqian,Zhang Qingchun,Duan Haigang,et al.Characteristic and favorable area prediction of Jurassic plays in Iraq[J].Xinjiang Petroleum Geology,2013,34(1):116-120.[周长迁,张庆春,段海岗,等.伊拉克侏罗系油气成藏组合特征及有利区预测[J].新疆石油地质,2013,34(1):116-120.]
[23]Yao Weijiang,Dang Yufang,Zhang Shuncun,et al.Formation of carboniferous reservoir in hongche fault belt,northwestern margin of Junggar Basin[J].Natural Gas Geoscience,2010,21(6):917-923.[姚卫江,党玉芳,张顺存,等.准噶尔盆地西北缘红车断裂带石炭系成藏控制因素浅析[J].天然气地球科学,2010,21(6):917-923.] 
[24]Li Yuying,Fu Xiaofei,Zhang Mingxue.Fault deformation features and rservoir-chtorlling mechanisms of Xujiangweizi Fault Depression in Songliao Basin[J].Natural Gas Geoscience,2012,23(6):979-988.[历玉英,付晓飞,张明学.松辽盆地徐家围子断陷断裂变形特征及控藏机理[J].天然气地球科学,2012,23(6):979-988.]
[25]Li Chunrong,Zhang Gongcheng,Liang Jianshe,et al.Characteristics of fault structure and its control on hydrocarbons in the Beibuwan Basin[J].Acta Petrolei Sinica,2012,33(2):195-203.[李春荣,张功成,梁建设,等.北部湾盆地断裂构造特征及其对油气的控制作用[J].石油学报,2012,33(2):195-203.]

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