准噶尔盆地车莫古隆起内物源沉积体系探讨及勘探意义——以白垩系清水河组一段为例
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摘要
为了探讨车莫古隆起对内物源沉积体系及油气成藏的控制作用,从车莫古隆起形成与演化入手,利用岩心、地震、测井等资料,多种方法结合恢复其剥蚀量、古地貌,提出车莫古隆起从中侏罗世到早白垩世发育,侏罗世末是其鼎盛时期,并提供内物源,控制围绕车莫古隆起周缘沉积体系和砂体展布,从岩心、地震特征、重矿物稳定系数、古水流指向、砂岩厚度等方面给出存在依据,合理解释了古隆起控制范围内已发现油藏的砂体成因。车莫古隆起发育和潜伏埋藏期控制古油气藏的形成与分布,掀斜后内物源砂体展布、断裂体系和现今构造共同控制着油气调整、运移及次生油气藏的分布,围绕车莫古隆起发育的内物源砂体尖灭方向与现今构造高部位指向垂直和斜交区域是岩性地层油气藏有利区。围绕内物源勘探刚开始,在此认识指导下部署的沙门1、莫17、夏盐11、夏盐12等井已获得突破,腹部岩性地层油气藏勘探将进入一个油气发现新阶段。
In order to reveal the main control factor of the distribution of depositional system and sandstone as well as its affection for reservoir forming,we have restored the palaeogeomorphology of Che-Mo paleo-uplift through a multi-method research based on the investigation of the coring,seismic and well logging data.The results indicate that Che-Mo paleo-uplift was developed from the Middle Jurassic to the Early Cretaceous and reached its peak development in the Late Jurassic.Information from the core,seismic section,heavy minerals,and sandbody thickness can also give a reasonable explanation about the origin mechanism of the reservoirs in this area.The distribution of depositional system and sandstone around Che-Mo paleo-uplift was controlled by local provenance sediments.The formation of ancient reservoirs was also determined by the appearance of this uplift.Tectonic movement including two structural tilting periods,the distribution of local provenance sandstone,fault system and modern structures are the key controlling factors for oil and gas migration and the formation of secondary reservoirs.We concluded that the area showing good correlation between local provenance sandstone and modern structures is favorable for the development of lithologic-stratigraphic reservoirs.The paleoslopes of Che-Mo paleo-uplift are the main regions for further exploration.This new understanding has brought a breakthrough in the exploration of Che-Mo paleo-uplift.Taking Shamen1 Well as an example,the exploration of lithologic-stratigraphic reservoirs in the central Junggar basin will enter a new period.
In order to reveal the main control factor of the distribution of depositional system and sandstone as well as its affection for reservoir forming,we have restored the palaeogeomorphology of Che-Mo paleo-uplift through a multi-method research based on the investigation of the coring,seismic and well logging data.The results indicate that Che-Mo paleo-uplift was developed from the Middle Jurassic to the Early Cretaceous and reached its peak development in the Late Jurassic.Information from the core,seismic section,heavy minerals,and sandbody thickness can also give a reasonable explanation about the origin mechanism of the reservoirs in this area.The distribution of depositional system and sandstone around Che-Mo paleo-uplift was controlled by local provenance sediments.The formation of ancient reservoirs was also determined by the appearance of this uplift.Tectonic movement including two structural tilting periods,the distribution of local provenance sandstone,fault system and modern structures are the key controlling factors for oil and gas migration and the formation of secondary reservoirs.We concluded that the area showing good correlation between local provenance sandstone and modern structures is favorable for the development of lithologic-stratigraphic reservoirs.The paleoslopes of Che-Mo paleo-uplift are the main regions for further exploration.This new understanding has brought a breakthrough in the exploration of Che-Mo paleo-uplift.Taking Shamen1 Well as an example,the exploration of lithologic-stratigraphic reservoirs in the central Junggar basin will enter a new period.
引文
[1]Peng X L.Query to Che-Mo paleo-uplift of Junggar Basin[J].China Petroleum Exploration,2007(6):63-70(in Chi-nese).
[2]Liu C R.No paleo-uplift of the Mesozoicin Middle of Junggar Basin[J].West Petroleum Exploration,2005,2(2):38-41(in Chinese).
[3]Zhao X,Yu X H,Huang X W,et al.Sequence stratigraphic characteristics of the First Member of Qingshuihe Formation in Shinan Area,Junggar Basin[J].Acta Sedimentologica Sin-ica,2007,25(5):716-721(in Chinese).
[4]Zhao H L.The evolution and reservoir,controlled patternin Chepaizi-Mosuowan paleo-uplift in Junggar Basin[J].Xin-jiang Petroleum Geology,2006,27(2):160-162(in Chi-nese).
[5]Wu X Z,Zhang N F,Shi X,et al.Structure characteristic and oil pattern of Che-Mo paleo-uplift in Junggar Basin[J].China Petroleum Exploration,2006(1):65-68(in Chinese).
[6]Tong DJ,Ren J Y,Ren YP.Evolution of Che-Mo paleo-up-lift control oil pool in Junggar Basin[J].Petroleum Geology and Recovery Efficiency,2006,13(3):39-42(in Chinese).
[7]He D F,Zhai G M,Kuang J,et al.Distribution and tectonic features of paleo-uplifts in the Junggar Basin[J].Chinese Journal of Geology,2005,40(2):248-261(in Chinese).
[8]Zhou L,Zheng J Y,Lei D W,et al.Recovery of eroded thickness of the Jurassic of Chemo palaeouplift in Junggar Ba-sin[J].Journal of Paleogeography,2007,9(3):244-252(in Chinese).
[9]Li P P,Zou H Y,Hao F.Formation mechanismand effect on petroleumaccumulation of the weathering crust,top of Ju-rassic,in the Hinterland of Junggar Basin[J].Acta Sedimen-tologica Sinica,2006,24(6):889-896(in Chinese).
[10]Li S J,Shi Y H,Wang Q C.The analysis of detrital heavy minerals in Cretaceous-Tertiary sandstones,Kuqa Depression and their implications for provenance[J],Acta Sedimentolog-ica Sinica,2006,24(1):28-35(in Chinese).
[11]Cao Y C,Wang YZ,Xu T Y,et al.Application of the ratio of characteristic elements in provenance analysis:A case study fromthe upper part of the fourth member of the Shahe-jie Fm.inthe W58area,Dongying Depression[J].Acta Sed-imentologica Sinica,2007,25(2):230-238(in Chinese).
[12]Zhao HG,Liu C Y.Approaches and prospects of provenanceanalysis[J].Acta Sedimentologica Sinica,2003,21(3):409-415(in Chinese).
[13]Hu P,Xu H,Li X B,et al.Sedimentary environments and the stratigraphic base-level cycle division of Jurassic coal measures in the East of Junggar Basin[J].Acta Sedimento-logica Sinica,2006,24(3):378-386(in Chinese).
[14]He Z H,Liu Z J,Zhang F.Latest progress of heavy mineral researchin the bas analysis[J].Geological Science and Tech-nology Information,2001,20(4):29-32(in Chinese).
[15]Chen C F,Zheng J M,Wang D F.Depositional systems and source provenance of the third member of Shahejie Formation in Banqiao Sag[J].Journal of Palaeogeography,2001,3(1):55-62(in Chinese).
[16]Li Z,Jiao Y Q,Liu C H,et al.Provenance analysis of heavy mineral in Gaoliu area of Huanghua Depression[J].Petrole-um Exploration and Development,1998,25(6):5-7(in Chi-nese).
[17]Got H,Monaco A,Vittori J,et al.Sedimentation on the Io-nian Zctive margin(Hellenic arc)provenance of sediments and mechanisms of deposition[J].Sedimentary Geology,1981,28(4):243-272.
[18]Li H Q.Interpretation of dipmeters in sedimentological re-search[J].Acta Sedimentologica Sinica,1995,13(1):82-87(in Chinese).
[19]Li J,Wang G W.Anew methodfor analyzing sandstone faci-es—Logging facies analysis[J].Geological Review,1996,42(5):443-447(in Chinese).
[1]彭希龄.准噶尔盆地车莫古隆起质疑[J].中国石油勘探,2007(6):63-70.
[2]刘朝荣.准噶尔盆地中部不存在中生代古隆起[J].西部油气勘探,2005,2(2):38-41.
[3]赵霞,于兴河,黄兴文,等.准噶尔盆地石南地区清水河组一段层序地层特征[J].沉积学报,2007,25(5):716-721.
[4]赵宏亮.准噶尔盆地车莫古隆起演化及其控藏规律[J].新疆石油地质,2006,27(2):160-162.
[5]吴晓智,张年富,石昕,等.准噶尔盆地车莫古隆起构造特征与成藏模式[J].中国石油勘探,2006(1):65-68.
[6]佟殿君,任建业,任亚平.准噶尔盆地车莫古隆起的演化及其对油气藏的控制[J].油气地质与采收率,2006,13(3):39-42.
[7]何登发,翟光明,况军,等.准噶尔盆地古隆起的分布与基本特征[J].地质科学,2005,40(2):248-261.
[8]周路,郑金云,雷德文,等.准噶尔盆地车莫古隆起侏罗系剥蚀厚度恢复[J].古地理学报,2007,9(3):244-252.
[9]李平平,邹华耀,郝芳.准噶尔盆地腹部侏罗系顶部风化壳的发育机制及其油气成藏效应[J].沉积学报,2006,24(6):889-896.
[10]李双建,石永红,王清晨.碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J].沉积学报,2006,24(1):28-35.
[11]操应长,王艳忠,徐涛玉,等.特征元素比值在沉积物物源分析中的应用——以东营凹陷王58井区沙四上亚段研究为例[J].沉积学报,2007,25(2):230-238.
[12]赵红格,刘池洋.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415.
[13]胡平,徐恒,李新兵,等.准噶尔盆地东部侏罗纪含煤岩系沉积环境及基准面旋回划分[J].沉积学报,2006,24(3):378-386.
[14]何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32.
[15]陈纯芳,郑浚茂,王德发.板桥凹陷沙三段沉积体系与物源分析[J].古地理学报,2001,3(1):55-62.
[16]李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998,25(6):5-7.
[18]李红奇.沉积学研究中的地层倾角测井资料解释[J].沉积学报,1995,13(1):82-87.
[19]李军,王贵文.一种分析砂岩沉积相的新方法——测井相分析[J].地质论评,1996,42(5):443-447.
[2]Liu C R.No paleo-uplift of the Mesozoicin Middle of Junggar Basin[J].West Petroleum Exploration,2005,2(2):38-41(in Chinese).
[3]Zhao X,Yu X H,Huang X W,et al.Sequence stratigraphic characteristics of the First Member of Qingshuihe Formation in Shinan Area,Junggar Basin[J].Acta Sedimentologica Sin-ica,2007,25(5):716-721(in Chinese).
[4]Zhao H L.The evolution and reservoir,controlled patternin Chepaizi-Mosuowan paleo-uplift in Junggar Basin[J].Xin-jiang Petroleum Geology,2006,27(2):160-162(in Chi-nese).
[5]Wu X Z,Zhang N F,Shi X,et al.Structure characteristic and oil pattern of Che-Mo paleo-uplift in Junggar Basin[J].China Petroleum Exploration,2006(1):65-68(in Chinese).
[6]Tong DJ,Ren J Y,Ren YP.Evolution of Che-Mo paleo-up-lift control oil pool in Junggar Basin[J].Petroleum Geology and Recovery Efficiency,2006,13(3):39-42(in Chinese).
[7]He D F,Zhai G M,Kuang J,et al.Distribution and tectonic features of paleo-uplifts in the Junggar Basin[J].Chinese Journal of Geology,2005,40(2):248-261(in Chinese).
[8]Zhou L,Zheng J Y,Lei D W,et al.Recovery of eroded thickness of the Jurassic of Chemo palaeouplift in Junggar Ba-sin[J].Journal of Paleogeography,2007,9(3):244-252(in Chinese).
[9]Li P P,Zou H Y,Hao F.Formation mechanismand effect on petroleumaccumulation of the weathering crust,top of Ju-rassic,in the Hinterland of Junggar Basin[J].Acta Sedimen-tologica Sinica,2006,24(6):889-896(in Chinese).
[10]Li S J,Shi Y H,Wang Q C.The analysis of detrital heavy minerals in Cretaceous-Tertiary sandstones,Kuqa Depression and their implications for provenance[J],Acta Sedimentolog-ica Sinica,2006,24(1):28-35(in Chinese).
[11]Cao Y C,Wang YZ,Xu T Y,et al.Application of the ratio of characteristic elements in provenance analysis:A case study fromthe upper part of the fourth member of the Shahe-jie Fm.inthe W58area,Dongying Depression[J].Acta Sed-imentologica Sinica,2007,25(2):230-238(in Chinese).
[12]Zhao HG,Liu C Y.Approaches and prospects of provenanceanalysis[J].Acta Sedimentologica Sinica,2003,21(3):409-415(in Chinese).
[13]Hu P,Xu H,Li X B,et al.Sedimentary environments and the stratigraphic base-level cycle division of Jurassic coal measures in the East of Junggar Basin[J].Acta Sedimento-logica Sinica,2006,24(3):378-386(in Chinese).
[14]He Z H,Liu Z J,Zhang F.Latest progress of heavy mineral researchin the bas analysis[J].Geological Science and Tech-nology Information,2001,20(4):29-32(in Chinese).
[15]Chen C F,Zheng J M,Wang D F.Depositional systems and source provenance of the third member of Shahejie Formation in Banqiao Sag[J].Journal of Palaeogeography,2001,3(1):55-62(in Chinese).
[16]Li Z,Jiao Y Q,Liu C H,et al.Provenance analysis of heavy mineral in Gaoliu area of Huanghua Depression[J].Petrole-um Exploration and Development,1998,25(6):5-7(in Chi-nese).
[17]Got H,Monaco A,Vittori J,et al.Sedimentation on the Io-nian Zctive margin(Hellenic arc)provenance of sediments and mechanisms of deposition[J].Sedimentary Geology,1981,28(4):243-272.
[18]Li H Q.Interpretation of dipmeters in sedimentological re-search[J].Acta Sedimentologica Sinica,1995,13(1):82-87(in Chinese).
[19]Li J,Wang G W.Anew methodfor analyzing sandstone faci-es—Logging facies analysis[J].Geological Review,1996,42(5):443-447(in Chinese).
[1]彭希龄.准噶尔盆地车莫古隆起质疑[J].中国石油勘探,2007(6):63-70.
[2]刘朝荣.准噶尔盆地中部不存在中生代古隆起[J].西部油气勘探,2005,2(2):38-41.
[3]赵霞,于兴河,黄兴文,等.准噶尔盆地石南地区清水河组一段层序地层特征[J].沉积学报,2007,25(5):716-721.
[4]赵宏亮.准噶尔盆地车莫古隆起演化及其控藏规律[J].新疆石油地质,2006,27(2):160-162.
[5]吴晓智,张年富,石昕,等.准噶尔盆地车莫古隆起构造特征与成藏模式[J].中国石油勘探,2006(1):65-68.
[6]佟殿君,任建业,任亚平.准噶尔盆地车莫古隆起的演化及其对油气藏的控制[J].油气地质与采收率,2006,13(3):39-42.
[7]何登发,翟光明,况军,等.准噶尔盆地古隆起的分布与基本特征[J].地质科学,2005,40(2):248-261.
[8]周路,郑金云,雷德文,等.准噶尔盆地车莫古隆起侏罗系剥蚀厚度恢复[J].古地理学报,2007,9(3):244-252.
[9]李平平,邹华耀,郝芳.准噶尔盆地腹部侏罗系顶部风化壳的发育机制及其油气成藏效应[J].沉积学报,2006,24(6):889-896.
[10]李双建,石永红,王清晨.碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J].沉积学报,2006,24(1):28-35.
[11]操应长,王艳忠,徐涛玉,等.特征元素比值在沉积物物源分析中的应用——以东营凹陷王58井区沙四上亚段研究为例[J].沉积学报,2007,25(2):230-238.
[12]赵红格,刘池洋.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415.
[13]胡平,徐恒,李新兵,等.准噶尔盆地东部侏罗纪含煤岩系沉积环境及基准面旋回划分[J].沉积学报,2006,24(3):378-386.
[14]何钟铧,刘招君,张峰.重矿物分析在盆地中的应用研究进展[J].地质科技情报,2001,20(4):29-32.
[15]陈纯芳,郑浚茂,王德发.板桥凹陷沙三段沉积体系与物源分析[J].古地理学报,2001,3(1):55-62.
[16]李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析[J].石油勘探与开发,1998,25(6):5-7.
[18]李红奇.沉积学研究中的地层倾角测井资料解释[J].沉积学报,1995,13(1):82-87.
[19]李军,王贵文.一种分析砂岩沉积相的新方法——测井相分析[J].地质论评,1996,42(5):443-447.
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