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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2009  >  31(1): 1-11
Wu Genyao, Liang Xing, Ma Li. TIME-SPATIAL DEVELOPING FEATURES OF CO-EXISTED INHERITED AND NEOGENIC STRUCTURES AND THEIR GUIDANCE TO MARINE ORIGIN OIL-GAS EXPLORATION IN THE YANGTZE CRATON[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(1): 1-11. doi: 10.11781/sysydz200901001
Citation: Wu Genyao, Liang Xing, Ma Li. TIME-SPATIAL DEVELOPING FEATURES OF CO-EXISTED INHERITED AND NEOGENIC STRUCTURES AND THEIR GUIDANCE TO MARINE ORIGIN OIL-GAS EXPLORATION IN THE YANGTZE CRATON[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(1): 1-11. doi: 10.11781/sysydz200901001
shu

TIME-SPATIAL DEVELOPING FEATURES OF CO-EXISTED INHERITED AND NEOGENIC STRUCTURES AND THEIR GUIDANCE TO MARINE ORIGIN OIL-GAS EXPLORATION IN THE YANGTZE CRATON

doi: 10.11781/sysydz200901001
  • 1.

    Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 2. Zhejiang Oilfield Company, China National Petroleum Corp., Hangzhou, Zhejiang 310013, China

  • 3. Jiangsu Oilfield, China Petroleum & Chemical Corp., Yangzhou, Jiangsu 225009, China

  • Received Date: 2008-06-05
  • Rev Recd Date: 2008-12-01
  • Publish Date: 2009-02-28
    Abstract
  • The study on time-spatial developing features of co-existed inherited and neogenic structures is an important step for the basin-orogeny coupling from a direction of petroliferous basin study to a guidance of oil-gas exploration.The exploration of marine origin oil-gas pool in China has taken a very tortuous road,and now it is in urgent need of new theoretical guiding.Taking the northern part of Upper Yangtze area(the Sichuan Basin) as an example,the paper described the orientation of structural line and its mechanism(coupled evolution with the neighbouring orogenic occurring) in the Precambrian,Caledonian,Hercynian-Indosinian and Yanshanian tectonic stages.A key knowledges for recent good progress of marine oil-gas exploration in the easetrn Sichuan Basin was lithologic-structural compound pool created by the Yanshanian neogenic structure(NE-orientation) acrossing the syn-marine sedimentary neogenic structure(NW-striking),which were named the 2nd and 3rd generation of neogenic structures respectively.In the western Sichuan Basin,the 3rd generation of neogenic structure was NEE-striking.To compare with eastern Sichuan,the paper analysed the orientation of structural line of each tectonic stage in the southern part of Upper Yangtze area(Guizhou) and Middle Yangtze area(Hubei) respectively.An obvious distinction in Guizhou might be that evolution of the epicontinental sea basin was coupled with the Babu-Phu Ngu ocean to the south(instead of the Qinling-Dabie ocean to thenorth of the Yangtze craton).In addition,Guizhou area was influenced by the plume tectonics in Late Permian-Early Triassic.The unique basemental structures(the N-S Huangling continental nucleus and the NE-striking Paleo-Tan-Lu fault zone) in Middle Yangtze area constrained the regional formation and deformation for a long time.Based on what mentioned above,the beneficial districts for marine oil-gas exploration in Guizhou and Hubei areas was discussed,which thought that the North Guizhou Basin(to the north of Guiyang-Anshun in west Guizhou) might be a hopeful area,although the orientations of Late Paleozoic and Mesozoic neogenic structures varied from the Sichuan Basin.

     

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    • References(74)
  • [1]
    张抗.从已发现的油气田看中国海相油气勘探[J].海相油气地质,2002,7(2):1～14
    [2]
    刘光鼎.中国油气资源企盼二次创业[J].地球物理学进展,2001,16(4):1～3
    [3]
    刘光鼎.雄关漫道真如铁——论中国油气二次创业[J].地球物理学进展,2002,17(2):185～190
    [4]
    朱德丰,任延广,吴河勇等.松辽盆地北部隐伏二叠系和侏罗系的初步研究[J].地质科学,2007,42(4):690～708
    [5]
    吴根耀.华南的格林威尔造山带及其坍塌:在罗迪尼亚超大陆演化中的意义[J].大地构造与成矿学,2000,24(2):112～123
    [6]
    吴根耀.从关键地质事件看华南的前寒武系划分[J].地层学杂志,2006,30(3):271～286
    [7]
    Wu G Y.Main tectonic units and geological evolution in South China and its environs:in the light of Gondwana dispersion and Asian accretion[A].In:Metcalfe I.Ed In Chief.Gondwana Dispersion and Asian Accretion[C].Rotterdam:A Balkema,1999.315～340
    [8]
    吴根耀,马力."盆""山"耦合和脱耦:含油气盆地研究的新思路[A].见:中国石油学会石油地质专业委员会编.油气盆地研究新进展第一辑[C].北京:石油工业出版社,2003.20～36
    [9]
    沈传波,梅廉夫.盆山体系与油气成藏作用[J].石油实验地质,2007,29(6):535～540
    [10]
    吴根耀,马力.试论"盆""山"耦合和脱耦研究的方法学[J].石油与天然气地质,2004,25(3):239～246
    [11]
    吴根耀.造山带古地理学——重建区域构造古地理的若干思考[J].古地理学报,2007,9(6):635～650
    [12]
    吴根耀,梁兴,叶舟.继承性构造与新生构造并存的时空发育特征及其油气勘探意义[J].现代地质,2008,22(5):766～778
    [13]
    陈洪德,庞林,倪新锋等.中上扬子地区海相油气勘探前景[J].石油实验地质,2007,29(1):13～18
    [14]
    丁道桂,刘光祥.扬子板内递进变形——南方构造问题之二[J].石油实验地质,2007,29(3):238～246
    [15]
    张士万,杨振武,梁西文等.中扬子海相天然气勘探层系及突破方向[J].石油实验地质,2007,29(4):361～366
    [16]
    周小进,杨帆.中国南方新元古代-早古生代构造演化与盆地原型分析[J].石油实验地质,2007,29(5):446～451
    [17]
    王津义,付孝悦,潘文蕾等.黔西北地区下古生界盖层条件研究[J].石油实验地质,2007,29(5):477～481
    [18]
    唐大卿,陈新军.川东北宣汉-达县地区断裂系统及构造演化[J].石油实验地质,2008,30(1):58～63
    [19]
    叶军.再议四川盆地西部坳陷深盆气[J].石油实验地质,2008,30(2):109～114
    [20]
    吴根耀.会理-东川裂堑的发育及形成机制[A].见:中国科学院地质研究所编著.1981届硕士学位论文集[C].北京:北京科学技术出版社,1983.80～90
    [21]
    罗志立,刘树根.中国塔里木、鄂尔多斯、四川克拉通盆地下古生界成藏条件对比分析[A].见:罗志立,李景明,刘树根等编.中国板块构造和含油气盆地分析[C].北京:石油工业出版社,2005.454～546
    [22]
    马永生,牟传龙,谭钦根等.关于开江-梁平海槽的认识[J].石油与天然气地质,2006,27(3):326～331
    [23]
    魏国齐,陈更生,杨威等.四川盆地北部开江-梁平海槽边界及特征初探[J].石油与天然气地质,2006,27(1):99～105
    [24]
    Wu G Y.Early Paleozoic accretion and amalgamation in a Gondwana-originated China[J].Acta Universitatis Carolinae-Geologica,1998,42(3～4):501～507
    [25]
    吴根耀.造山带地层学[M].成都;乌鲁木齐:四川科学技术出版社;新疆科学技术出版社,2000.218
    [26]
    Wu Genyao.Rejuvenation of fossil sutures and related Mesozoic intracontinental orogens in South China[J].Acta Geologica Sinica,2000,74(2):194～200 (中文稿 "古缝合线活化和华南中生代陆内造山运动"见:中国地质学会编.第31届国际地质大会中国代表团学术论文集[C].北京:地质出版社,2001.32～39)
    [27]
    吴根耀.燕山运动和中国大陆晚中生代的活化[J].地质科学,2002,37(4):453～461
    [28]
    梁新权,郭定良.湖南深部构造活化及其浅部响应[J].地质科学,2002,37(3):332～342
    [29]
    吴根耀,马力.中国南方"盆""山"耦合和脱耦关系[A].见:马力,陈焕疆,甘克文等著.中国南方大地构造和海相油气地质[M].北京:地质出版社,2004.180～255
    [30]
    罗志立.试从板块构造探讨四川盆地新的油气资源[J].石油勘探与开发,1975,(6):5～27
    [31]
    安作相.塔里木-华南地块裂解与四川下古生界油气[J].石油学报,1997,18(1):18～22
    [32]
    王金琪.四川盆地油气地质特征——纪念黄汲清先生百岁诞辰[J].石油实验地质,2004,26(2):115～120
    [33]
    王一刚,陈盛吉,徐世琦.四川盆地古生界-上元古界天然气成藏条件及勘探技术[M].北京:石油工业出版社,2001.67～78
    [34]
    魏国齐,杨威,吴世祥等.四川盆地北部开江-梁平海槽边界厘定及其油气勘探意义[A].见:中国石油地质年会学术委员会编.中国石油地质年会论文集[C].北京:石油工业出版社,2005.319～325
    [35]
    李三忠,赖绍聪,张国伟等.秦岭勉(县-)略(阳)缝合带及南秦岭地块的变质动力学研究[J].地质科学,2003,38(2):137～154
    [36]
    胡健民,赵国春,马国良等.秦岭造山带武当地区古生代伸展构造[J].地质科学,2004,39(3):305～319
    [37]
    马永生,蔡勋育,李国雄.四川盆地普光大型气藏基本特征及成藏富集规律[J].地质学报,2005,79(6):858～865
    [38]
    马永生,蔡勋育.四川盆地川东北区二叠系-三叠系天然气勘探成果与前景展望[J].石油与天然气地质,2006,27(6):741～750
    [39]
    Wu Genyao,Yano T,Inomata M.Yanshanian orogenics in South China:a relation to Neotethyan evolution[J].Scientia Geologica Sinica,1998,7(1):1～10
    [40]
    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
    [41]
    吴根耀,矢野孝雄.东亚大陆边缘的构造格架及其中-新生代演化[J].地质通报,2007,26(7):787～800
    [42]
    王金琪.小陆拼接、多旋回、陆内构造——中国大陆石油地质三根基柱[J].成都理工学院学报,1998,25(2):182～190
    [43]
    黄泽光,刘光祥,潘文蕾等.川西坳陷压扭应力场的形变特征及油气地质意义[J].石油实验地质,2003,25(6):701～707
    [44]
    曹伟.龙门山推覆构造带中段前缘构造浅析[J].石油实验地质,1994,16(1):35～40
    [45]
    蔡立国.四川前陆褶皱-冲断带构造样式与特征[J].石油实验地质,1997,19(2):115～120
    [46]
    李亚林,张国伟,李三忠等.秦岭略阳-白水江地区双向推覆构造及形成机制[J].地质科学,2001,36(4):465～473
    [47]
    何建坤,卢华复,张庆龙等.南大巴山冲断构造及其剪切挤压动力学机制[J].高校地质学报,1997,3(4):419～428
    [48]
    张进江,郑亚东,刘树文.小秦岭金矿田中生代构造演化与矿床形成[J].地质科学,2003,38(1):74～84
    [49]
    孙晓猛,吴根耀,郝福江等.秦岭-大别造山带北部中-新生代逆冲推覆构造期次及时空迁移规律[J].地质科学,2004,39(1):63～76
    [50]
    岳东明.浅析川西坳陷燕山中晚期构造圈闭的有效性[J].石油实验地质,1999,21(4):336～340
    [51]
    吴根耀,马力."盆""山"耦合和脱耦在含油气盆地分析中的应用[J].石油实验地质,2003,25(6):648～660
    [52]
    钟大赉,吴根耀,季建清等.滇东南发现蛇绿岩[J].科学通报,1998,43(13):1365～1370
    [53]
    Tran Q H,Poliakov G V,Balykin P A,et al.Ultramafic-mafic associations and related mineralization in northern Vietnam[J].Journal of Geology,series B,1995,(5-6):434～435
    [54]
    Wu Genyao,Zhong Dalai,Zhang Qi,et al.Babu-Phu Ngu ophiolite:A geological record of Paleotethyan ocean bordering China and Vietnam[J].Gondwana Research,1999,2(4):554～557
    [55]
    吴根耀,马力,钟大赉等.滇桂交界区印支期增生弧型造山带:兼论与造山作用耦合的盆地演化[J].石油实验地质,2001,23(1):8～18
    [56]
    吴根耀.滇桂交界区印支期前陆褶皱冲断带[J].地质科学,2001,36(1):64～71
    [57]
    Wu Genyao.Indosinian foreland fold-and-thrust belt bordering Yunnan and Guangxi,China[J].Acta Geologica Sinica,2001,75(4):391～397
    [58]
    索书田,侯光久,张明发等.黔西南盘江大型多层次席状逆冲-推覆构造[J].中国区域地质,1993,(3):239～247
    [59]
    吴根耀.古深断裂活化与燕山期陆内造山运动——以川南-滇东和中扬子褶皱-冲断系为例[J].大地构造与成矿学,2001,25(3):246～253
    [60]
    丘元禧,陈焕疆主编.云开大山及其邻区地质构造论文集[M].北京:地质出版社,1993.1～11,44～52
    [61]
    吴根耀,马力,许效松等.喜马拉雅运动:对川滇交界区古地理重建的制约和楚雄盆地的改造[J].古地理学报,2001,3(2):3～10
    [62]
    张进江,钟大赉,桑海清等.哀牢山-红河构造带古新世以来多期活动的构造和年代学证据[J].地质科学,2006,41(2):291～310
    [63]
    王晓鹏,吴根耀,钟大赉.受红河断裂控制的晚第三纪走滑松弛盆地——以漠沙盆地为例[J].地质科学,2001,36(3):370～379
    [64]
    吴根耀,陈焕疆,马力等.中国东部燕山期高原的发育及对矿产和油气资源评价的启示[J].石油实验地质,2002,24(1):3～12
    [65]
    吴根耀,陈焕疆,马力等.苏皖地块——特提斯演化阶段独立的构造单元[J].古地理学报,2002,4(2):77～86
    [66]
    吴根耀.白垩纪:中国及邻区板块构造演化的一个重要变换期[J].中国地质,2006,33(1):64～77
    [67]
    许德如,贺转利,李鹏春等.湘东北地区晚燕山期细碧质玄武岩的发现及地质意义[J].地质科学,2006,41(2):311～332
    [68]
    吴根耀,马力,陈焕疆等.苏皖地块构造演化、苏鲁造山带形成及其耦合的盆地发育[J].大地构造与成矿学,2003,27(4):337～353
    [69]
    柳祖汉.湘中-南地区二叠系沉积相的分异及成因[J].地质科学,2005,40(4):510～517
    [70]
    吴根耀,马力.试论"盆""山"耦合和脱耦及其运动学[J].石油实验地质,2003,25(2):99～109,115
    [71]
    李双应,王道轩,刘因等.大别造山带折返剥露历史:来自合肥盆地南缘中生界变质岩碎屑的证据[J].地质科学,2005,40(4):518～531
    [72]
    吴根耀.湘鄂赣皖交界区的湖盆演化及其控制因素[J].大地构造与成矿学,1997,21(3):251～261
    [73]
    徐政语,林舸,刘池阳等.从江汉叠合盆地构造形变特征看华南与华北陆块的拼贴过程[J].地质科学,2004,39(2):284～295
    [74]
    吴根耀.中国滇西-泰国地区侏罗纪-第四纪盆地发育及其对比研究[J].地质科学,1991,26(4):359～368
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