塔里木盆地巴楚-麦盖提地区古构造演化及其对奥陶系储层发育的控制作用
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
依据2D和3D地震资料解释及钻井分层数据得到的不同时代地层的残余厚度图和现今埋深图,在对主要构造不整合面剥蚀量恢复和去压实校正的基础上,采用古构造、古地貌恢复方法,利用盆地模拟软件(PetroMod10)计算了不同地层的在不同构造时期的古埋深和古厚度,系统深入研究了巴楚-麦盖提地区古构造演化历史,阐明了巴楚隆起与和田古隆起构造演化关系及迁移规律,结合奥陶系岩溶储层发育特征,探讨了古隆起演化与岩溶储层发育之间关系,建立了岩溶储层发育的构造演化模式,预测了奥陶系有利岩溶储层分布地区。结果表明:巴楚-麦盖提地区古构造演化经历了加里东期、海西期、印支-燕山期和喜山期等4个构造旋回阶段;不同时期古构造面貌受控于不同构造期的区域构造应力场变化,巴楚隆起是海西早期开始发育,显现出隆起的雏形,到喜山中期开始大幅度隆升,并最终定型。构造演化经历了二个阶段,即海西运动的隆起形成和喜山运动强烈隆升改造阶段,隆起位置迁移不明显,主要表现在隆起规模上的变化。而和田古隆起则是在加里东期-海西期发育的一个大型古隆起,现今呈现为一个向南倾斜的大型麦盖提斜坡带;构造演化经历了早加里东运动雏形形成、加里东中期-海西早期运动持续隆升、海西运动中晚期的沉降埋藏、印支-喜马拉雅运动期的掀斜消失等四个阶段,且古隆起位置在平面上发生了明显逆时针方向的迁移。受和田古隆起构造演化的控制,奥陶系发育了加里东中期、晚期和海西早期等三期风化壳岩溶,其中以海西早期岩溶最发育;玉北地区遭受了三期构造抬升剥蚀,为三期岩溶的叠置区,是巴楚-麦盖提地区岩溶储层发育的最有利地区。
Basd on the residual thickness map and present buried depth map of different strata interpreted from 2D and 3D seismic data and drilling data,after recovery of erosion amounts of main structural uncomformity surface and strata compaction correction,the paleo-structure,paleogeomorphologic restoration method and basin modeling software are employed to calculate the paleo-buried depth and the thickness of different formations during different tectonic periods. This paper also systematically studies on the tectonic evolution history in Bachu-Markit region,and illustrates tectonic evolution and migration of the Bachu and Hetian ancient uplift. The Ordovician karst reservoir is characterized,and its relation to ancient uplift evolution is discussed. Tectonic evolution model of the development of karst reservoir is established to forecast the favorable distribution area for Ordovician karst reservoir. The results show that Bach-Markit ancient tectonic experienced four stages of tectonic cycle,including Caledonian stage,Hercynian stage,Indosinian- Yanshan stage and Himalayan stage; tectonic appearance is controlled by the changes of regional tectonic stress field of different geologic period,Bachu uplift began to develop in the Early Hercynian and form the prototype of the uplift. Until to the Himalayan it substantially uplifted,and finally came into its present shape. The structural evolution experienced two stages,namely the uplift formation by the stage Hercynian Movement and the strong transformation by the stage Himalayan Movement,but the migration of uplift position is subtle,which appears as the change of uplift scale. However,the Hetian ancient uplift is a large ancient uplift which developed in Caledonian-Hercynian,now appears as a large slope belt named as Markit tilted to the south; The structural evolution experienced three stages,including the formation of embyro during the stage Hercynian Movement and the Continued uplift stage in Himalayan Movement,the settlement burial stage in Middle-Late Hercynian Movement and the tilt transformation and extinction stage during Himalayan Movement. The position of the ancient uplift obviously changed in the plane by moving counterclockwise. Being controlled by the tectonic evolution of Hetian ancient uplift,the Ordovician developed three stages about weathered crust of karst, including the Middle Caledonian,the Late Caledonian and the Early Hercynian,among which karst in Early Hercynian was the most developed; And the region of Yubei,suffered three stages of structural tectonic uplift,was the overlapped area owning three stage of Karst,and therefore is proved to be the most favorable area of the development of the karst reservoir in Bachu-Markit.
引文
Allen PA and Allen JR.1990.Basin Analysis Principles and Applications.London:Blackwell Scientific Publications
    Chen ZN,Wang XM,Chen S et al.2008.Structural evolution of Fuyureservoir in the Chaochang area of Songlioa basin.Geoscience,22(4):512-519(in Chinese with English abstract)
    Dahlstrom CDA.1969.Balanced cross sections.Canadian Journal ofEarth Sciences,6:743-757
    Ding WL,Lin CS,Qi LX et al.2008.Structural framework and evolutionof Bachu uplift in Tarim basin.Earth Science Frontiers,15(2):242-252(in Chinese with English abstract)
    Feng YZ,Song WQ and Liu SY.2007.Study and application of ancientlanform recovering method using geological data.Journal ofStratigraphy,31(Suppl.Ⅱ):527-531(in Chinese with Englishabstract)
    Gibbs AD.1983.Balanced cross-section construction from seismicsections in areas of extensional tectonics.Journal of StructuralGeology,5:153-160
    Guo SB and Sun SH.2006.Rebuilding paleogeomorphology of PreJurassic and oil-gas accumulation regulation in Zhoujiawan area.Earth Science,31(3):372-377(in Chinese with Englishabstract)
    He DF,Jia CZ,Li DS et al.2005.Formation and evolution of polycyclicsuperimposed Tarim basin.Oil&Gas Geology,26(1):64-77(inChinese with English abstract)
    He DF,Zhou XY,Yang HJ et al.2008.Formation mechanismandtectonic types of intracratonic paleo-uplifts in the Tarim basin.EarthScience Frontiers,15(2):207-221(in Chinese with Englishabstract)
    He MX and Liu CY.1992.The Analysis of Strike-slip Deformation andPaleo-structure in Basin.Xian:Northwest University Press(inChinese)
    He WY,Li JH,Qian XL et al.2000.The Meso-Cenozoic evolution ofBachu fault-uplift in Tarim basin.Acta Scicentiarum NaturalumUniversitis Pekinesis,36(4):539-545(in Chinese with Englishabstract)
    Jia CZ,Wei GQ,Yao HJ et al.1995.Basin tectonic evolution andregional tectonic geology.In:Tong XG and Liang DG(eds.).Series of Oil and Gas Exploration in Tarim Basin.Beijing:PetroleumIndustry Press(in Chinese)
    Kang YZ and Kang ZH.1994.Tectonic evolution and oil and gas ofTarim basin.Bulletin of the Chinese Academy of GeologicalSciences,3(4):180-191(in Chinese)
    Kang ZH and Wu MD.2003.Technology of recovering ancient geomorphythrough sequence stratigraphy:A case study in Tahe6threservoir,Tarim Basin.Xinjiang Geology,21(3):290-292(in Chinese withEnglish abstract)
    Kang ZH.2006.The karst palaeogeomorphology of carbonate reservoir inTahe Oilfield.Xinjiang Petroleum Geology,27(5):522-525(inChinese with English abstract)
    Li YJ,Mai GR,Luo JC et al.1999.Palaeozoic tectonic setting andprovenance nature discrimination of Bachu fault-uplift,Tarim,Northwest China.Journal of Palaeogeography,1(4):45-52(inChinese with English abstract)
    Li ZJ and Wang QC.2002.Method and technique for prediction of super-deep carbonate reservoirs in north Tarim basin.Oil and GasGeology,21(5):35-40(in Chinese with English abstract)
    Liu GB,Shi ZJ and She XY.2004.Regional tectonic evolution anddistribution of Bachu-Markit.Journal of Chengdu University ofTechnology(Science and Technology Edition),36(2):157-161(in Chinese with English abstract)
    Liu WJ,Zheng RC and Li XH.1999.Reconstruction of palaeogeographyand palaeotectonics of a Devonian sedimentary basin in Longmenshanarea,Sichuan.Acta Geologica Sinica,73(2):109-119(inChinese with English abstract)
    Liu XF,He YB and Zhang HD.1999.Palaeotectonic reconstructionusing backstripping analysis:Example from the border areas ofSichuan,Hubei and Hunan provinces.Journal of Palaeogeography,1(2):53-61(in Chinese with English abstract)
    Liu XF,Meng LK,Zhao CY et al.2003.Method for basin palaeotectonicreconstruction based on GIS.Geomatics and Information Science ofWuhan University,28(2):197-207(in Chinese with Englishabstract)
    Lou D,Li SZ,Jin C et al.2008.Evolution of the Mesozoic strata in themiddle range of the Huanghua depression.Marine Geology andQuaternary Geology,28(3):43-53(in Chinese with Englishabstract)
    Ma RH and Wang AZ.2006.Mapping palaeostructural evolution withtectonic reconstruction theory.Natural Gas Industry,26(1):3436(in Chinese with English abstract)
    Pang YJ,Dai ZY,Liu SH et al.2007.Restoration method of Ordovicianweathering crust paleo-geomorphology of Leshan-Longnv templepaleohigh and its features in central Sichuan.Petroleum Geology andEngineering,21(5):8-15(in Chinese with English abstract)
    Qi JF,Yang Q and Wang ZY.2003.Some problems about compiling arestored paleo-structural map of basin.Chinese Journal of Geology,38(3):413-424(in Chinese with English abstract)
    Ren Y.2002.Ancient structural evolution of hadrocarbon accumulationin southeastern part of giant synclise of Caspian seashore basin.Xinjiang Petroleum Geology,23(4):351-354(in Chinese withEnglish abstract)
    Rowan MG and Linares R.2000.Fold-evolution matrices and axialsurface analysis of fault-bend folds:Application to the Medinaanticline eastern Cordillera,Columbia.AAPG Bulletin,84(6):741-764
    Shaw JH and Suppe J.1994.Structural trend analysis by axial surfacemapping.AAPG Bulletin,78(5):700-721
    Shi YM,Chen GP,Pan JG et al.2004.Application of comprehensivereservoir prediction techniques to the carbonate rocks in Tarim basin.Natural Gas Industry,24(12):51-53(in Chinese with Englishabstract)
    Song GQ,Xu CH,Fan QZ et al.2000.Sequence stratigraphy applied inthe restoration of the Caledonian paleogeomorphy.ExperimentalPetroleum Geology,22(4):351-354(in Chinese with Englishabstract)
    Suppe J.1983.Geometry and kinematics of fault-bend folding.AmericanJournal of Science,28(3):684-721
    Wagoner JC.1985.Reservoir facies distribution as controlled by sea-levelchange.Society of Economic Paleontologists and Mineralologists,91-92
    Wang JH,Wang H,Zhao ZX et al.2003.Sequence stratigraphy inpaleogeomorphy analysis.Earth Science,28(4):425-430(inChinese with English abstract)
    Wang QH.1999.Structural characteristics and its control on reservoirdistribution in Bachu arch,Tarim basin.Xinjiang PetroleumGeology,20(3):208-209(in Chinese with English abstract)
    Xu JY,Wang YP and Wang L.1997.Reconstruction of3-Dpaleostructures of multi-axis horizontal extensive basin.Oil and GasGeology,18(1):1-5(in Chinese with English abstract)
    Xu XK,Liu SG,Li J et al.2003.Haixi paleogeomorphology on Hetianpalaeohigh.Special Oil and Gas Reservoirs,10(3):142-148(inChinese with English abstract)
    Zhao JX,Chen HD,Shi ZQ.2001.The way and implications of rebuilding paleogeomorphology:Taking the research of palaeogeomorphology the Ordos Basin before Jurassic deposition as example.Journal of Chengdu University of Technology,28(3):260-266(inChinese with English abstract)
    Zhao JX,Chen HD and Xiang F.2003.The possibility of rebuildingpaleogeomorphology befores basin deposition by high resolutionsequence stratigraphy.Journal of Chengdu University of Technology(Science and Technology Edition),30(1):76-81(in Chinesewith English abstract)
    Zhu GY,Zhang SC,Liang YB et al.2005.Isotopic evidence of TSRorigin for natural gas bearing high H2S contents within theFeixianguan Formation of the northeastern Sichuan Basin,southwestern China.Science in China,48(11):1960-1971
    Zhu GY,Zhang SC,Liang YB et al.2006.Dissolution and alteration ofthe deep carbonate reservoirs by TSR:An important type of deepburied high-quality carbonate reservoirs in Sichuan Basin.ActaPetrologica Sinica,22(8):2182-2194(in Chinese with Englishabstract)
    Zhu GY,Zhao WZ,Liang YB et al.2007.Discussion of gas enrichmentmechanism and natural gas origin in marine sedimentary Basin,China.Chinese Science Bulletin,52(Suppl.),62-76
    Zhu GY and Zhang SC.2009.Hydrocarbon accumulation conditions andexploration potential of deep reservoirs in China.Acta PetroleiSinica,30(6):793-802(in Chinese with English abstract)
    Zhu GY,Zhang SC,Wang HH et al.2009.Forming and distribution ofdeep weathering crust reservoir in North Tarim basin.ActaPetrologica Sinica,25(10):2384-2398(in Chinese with Englishabstract)
    Zhu GY,Zhang SC,Zhang B et al.2010.Reservoir types of marinecarbonates and their accumulation model in western and centralChina.Acta Petrolei Sinica,31(6):871-878(in Chinese withEnglish abstract)
    Zhu GY,Jiang NH,Su J et al.2011a.The formation mechanism of highdibenzothiophene series concentration in Paleozoic crude oils fromTazhong area,Tarim basin,China.Energy Exploration&Exploitation,29(5):617-632
    Zhu GY,Zhang SC,Huang HP et al.2011b.Gas genetic type and originof hydrogen sulfide in the Zhongba gas field of the western SichuanBasin,China.Applied Geochemistry,26:1261-1273
    Zhu GY,Yang HJ,Zhu YF et al.2011.Study on petroleum geologicalcharacteristics and accumulation of carbonate reservior in Hanilcatamarea,Tarim Basin.Acta Petrologica Sinica,27(3):827-844(inChinese with English abstract)
    Zhu GY,Cui J,Su J et al.2012.Accumulation and reformation ofSilurian reservoir in the northern Tarim Basin.Acta GeologicaSinica,86(1):209-225
    Zhu GY,Yang HJ,Su J et al.2012a.True exploration potential ofmarine oils in the Tarim Basin.Acta Petrologica Sinica,28(4):1333-1347(in Chinese with English abstract)
    Zhu GY,Yang HJ,Su J et al.2012b.New progress of marinehydrocarbon Geological theory in China.Acta Petrologica Sinica,28(3):722-738(in Chinese with English abstract)
    陈昭年,王小敏,陈珊等.2008.松辽盆地朝长地区扶余油层的构造演化.现代地质,22(4):512-519
    丁文龙,林畅松,漆立新等.2008.塔里木盆地巴楚隆起构造格架及形成演化.地学前缘,15(2):242-252
    冯延状,宋维琪,刘仕友.2007.利用地震资料进行古地貌恢复方法研究及应用.地层学杂志,31(增Ⅱ):527-531
    郭少斌,孙绍寒.2006.周家湾地区前侏罗纪古地貌恢复及油气富集规律.地球科学,31(3):372-377
    何登发,贾承造,李德生等.2005.塔里木盆地多旋回叠合盆地的形成与演化.石油与天然气地质,26(1):64-77
    何登发,周新源,杨海军等.2008.塔里木盆地克拉通内古隆起的成因机制与构造类型.地学前缘,15(2):207-221
    何明喜,刘池洋.1992.盆地走滑变形研究与古构造分析.西安:西北大学出版社
    何文渊,李江海,钱祥麟等.2000.塔里木盆地巴楚断隆中新生代的构造演化.北京大学学报(自然科学版),36(4):539-545
    贾承造,魏国齐,姚慧君等.1995.盆地构造演化与区域构造地质.见:童晓光,梁狄刚编.塔里木盆地油气勘探丛书.北京:石油工业出版社
    康玉柱,康志宏.1994.塔里木盆地构造演化与油气.地球学报,3(4):180-191
    康志宏,吴铭东.2003.利用层序地层学恢复岩溶古地貌技术——以塔河油田6区为例.新疆地质,21(3):290-292
    康志宏.2006.塔河碳酸盐岩油藏岩溶古地貌研究.新疆石油地质,27(5):522-525
    李曰俊,买光荣,罗俊成等.1999.塔里木盆地巴楚断隆古生代沉积构造背景和物源区性质的探讨.古地理学报,1(4):45-52
    李宗杰,王勤聪.2002.塔北超深层碳酸盐岩储层预测方法和技术.石油与天然气地质,23(1):35-40
    刘高波,施泽进,佘晓宇.2004.巴楚-麦盖提的区域构造演化与油气分布规律.成都理工大学学报(自然科学版),31(2):157161
    刘文均,郑荣才,李祥辉.1999.龙门山泥盆纪沉积盆地的古地理和古构造重建.地质学报,73(2):109-119
    刘学锋,何幼斌,张或丹.1999.利用回剥分析重建古构造格局——以川、鄂、湘边区为例.古地理学报,1(2):53-61
    刘学锋,孟令奎,赵春宇等.2003.基于GIS的盆地古构造重建方法研究.武汉大学学报(信息科学版),28(2):197-207
    楼达,李三忠,金宠等.2008.黄骅坳陷中区中生代构造演化.海洋地质与第四纪地质,28(3):43-53
    马如辉,王安志.2006.利用构造恢复原理制作古构造演化图.天然气工业,26(1):34-36
    庞艳君,代宗仰,刘善华等.2007.川中乐山-龙女寺古隆起奥陶系风化壳地貌恢复方法及其特征.石油地质与工程,21(5):815
    漆家福,杨桥,王子煜.2003.编制盆地复原古构造图的若干问题的讨论.地质学报,38(3):413-424
    任俞.2002.滨里海巨型台向斜东南部油气聚集的古构造条件.新疆石油地质,23(4):351-354
    师永民,陈广坡,潘建国等.2004.储层综合预测技术在塔里木盆地碳酸盐岩中的应用.天然气业,24(12):51-53
    宋国奇,徐春华,樊庆真等.2000.应用层序地层方法恢复加里东期古地貌——以济阳坳陷沾化地区为例.石油实验地质,,22(4):351-354
    王家豪,王华,赵忠新等.2003.层序地层学应用于古地貌分析——以塔河油田为例.地球科学,28(4):425-430
    王清华.1999.塔里木盆地巴楚凸起构造特征及其对油气藏分布的控制.新疆石油地质,20(3):208-209
    徐希坤,刘树根,黎剑等.2003.和田古隆起海西早期古地貌恢复.特种油气藏,10(3):32-34
    许浚远,王艳萍,王磊等.1997.多轴水平拉伸盆地三维古构造重建探讨.石油与天然气地质,18(1):1-5
    赵俊兴,陈洪德,时志强.2001.古地貌恢复技术方法及其研究意义——以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例.成都理工学院学报,28(3):260-266
    赵俊兴,陈洪德,向芳.2003.高分辨率层序地层学方法在沉积前古地貌恢复中的应用.成都理工大学学报(自然科学版),30(1):76-81
    朱光有,张水昌,梁英波等.2006.TSR对深部碳酸盐岩储层的溶蚀改造作用——四川盆地深部碳酸盐岩优质储层形成的重要方式.岩石学报,22(8):2182-2194
    朱光有,张水昌.2009.中国深层油气成藏条件与勘探潜力.石油学报,30(6):793-802
    朱光有,张水昌,王欢欢等.2009.塔里木盆地北部深层风化壳储层的形成与分布.岩石学报,25(10):2384-2398
    朱光有,张水昌,张斌等.2010.中国中西部地区海相碳酸盐岩油气藏类型与成藏模式.石油学报,31(6):871-878
    朱光有,杨海军,朱永峰等.2011.塔里木盆地哈拉哈塘地区碳酸盐岩油气地质特征与富集成藏特征.岩石学报,27(3):827-844
    朱光有,杨海军,苏劲等.2012a.塔里木盆地海相石油的真实勘探潜力.岩石学报,28(4):1333-1347
    朱光有,杨海军,苏劲等.2012b.中国海相油气地质理论新进展.岩石学报,28(3):722-738

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心