Wu Genyao. A TECTONIC OUTLOOK OF MOBILISM ON BASIN STUDY[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1998, 20(4): 309-318. doi: 10.11781/sysydz199804309
Citation: Wu Genyao. A TECTONIC OUTLOOK OF MOBILISM ON BASIN STUDY[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1998, 20(4): 309-318. doi: 10.11781/sysydz199804309

A TECTONIC OUTLOOK OF MOBILISM ON BASIN STUDY

doi: 10.11781/sysydz199804309
  • Received Date: 1997-12-27
  • Publish Date: 1998-10-25
  • A short review of history on the oil and gas-bearing basin study reveals the development to experience a zigzag path of structural-sedimentory-tectonic researches.The recent contributions of petroleum geology should be attributed to the plate tectonics.To face a grim situation of oil and gas exploration,we should develop and perfect the tectonic outlook of mobilism,which is a guiding ideology and theoretical instruction on basin study.In the process of basin occurring and sediments depositing,the following changes can be observed in a basin:(1) the basin geometry and framework,(2) the inner textures,(3) the growth structures,(4) the tectonic setting and provenance,(5) the basin type and its formation,and (6) the geothermal pattern.Spatially,the basin analysis of mobilism is expressed by the following relationships:(1) the part and the whole of a basin,(2) a single basin and the basin group,(3) the regional and the local stress fields,and (4) the tectonic styles in the shallow and the deep.In addition,the complexities of continental margins and geothermal fields should be emphasized.A unitedly kinematic process and dynamic mechanics between orogenics and basin evolution can be explored from the viewpoints of (1) compression and tension being interdependent,(2) transformation by strike-slip faults,and (3) deep-seated courses.To comprehend the basin occurring,sedimentation and thermal action,the three efforts should be ma ken greatly:(1) to sum up the features of basin evolution related to the global tectonic cycles,(2) to take tectonics as a key link and to synthesize the knowledges of structural geology,sequence stratigraphy,sedimentology,geochemistry,geothermology,groundwater dynamics and oil-gas accumulation dynamics,and (3) to understand the reformation or influence of the youngest tectono-thermal event.

     

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  • [1]
    朱夏.论中国含油气盆地构造.北京:石油工业出版社,1986.
    [2]
    甘克文.沿着朱夏教授开拓的道路发展含油气盆地地质学的理论,为深化我国的油气勘探作出贡献.孙肇才、张渝冒主编.中国油气盆地分析-朱夏学术思想研讨文集.北京:石油工业出版社,1993,122-127.
    [3]
    甘克文.油气盆地研究中的一个基本问题——构造学研究.丁贵时,甘克文,郑俊章,潘校华,王玉新等编.油气勘探工程新进展(一).北京:石油工业出版社,1995,6-14.
    [4]
    Wu G Y.Collision tectonics in the central sector of the Sanjiang Indosinides bordering Xizang(Tibet),Sichuan and Yunnan,China.Proceedin gs of the International Conference on Stratigraphy and Tectonic Evolution of Southeast Asia and South Pacific,Ban gkok,Thailand,Aug.1997,347~359.
    [5]
    Bhattacharjee C C.The ophiolites of northeast India:a su bduction zone ophiolite complex of the India-Burma orogenic belt.Tectonop hysics,1991,191:213~222.
    [6]
    Ricci Lucchi F.Petroleum exploration worldwide,a history of advsnces since 1950 and a look at future targets.Tulsa:Penn well,1986.
    [7]
    ??±é?3??.?o??à3í?1à?í1???o.???o′?±μ:《??μ?±》,1977.
    [8]
    张文佑、吴根耀.裂谷构造与成矿作用.大自然探索,1982,1(2):13~33.
    [9]
    Yano T,Wu G Y,Tan M Q and Sha S L.Tectono-sedimentary development of backarc continental bas in in Yunnan,southern China.Journal of SE Asian Earth Science,1994,9:153~166.
    [10]
    Milanovsky E E.Classification and evolution of continental rifts.Tectonophysics,1972,15:65~70.
    [11]
    张文佑.断块构造导论.北京:石油工业出版社,1984.
    [12]
    Bender F.Geology of Burma.Ber lin:Gebr der Bonntraeger,1983.
    [13]
    张文佑、吴根耀.试论碰撞构造——一种假说性的探讨.大自然探索,1986,5(1):97~104.
    [14]
    Nelson K D.Are crustal thickness variations in old mountain belts like the Appalachians a consequence of lith os pheric delamination?Geology,1992,20:498~502.
    [15]
    Sacks P E and Secor D T jr.Delamination in collisional orogens.Geology,1990,18:999~1002.
    [16]
    Vail P R,Audemard F,Bowman S A,Einsele G and Perez G.The stratigraphic signatures of tectonis,eustasy and sedimen tation.in:G Einsele,W Ricken and A Seilacher,(eds.),Cycles and Events in Stratigraphy.Berlin:Springer-Verlag,1991,617~659.
    [17]
    吴根耀.张文佑教授与油气田地质学.石油学报,1987,8(3):1~6.
    [18]
    陈发景.学习朱夏教授学术思想,积极开展含油气盆地的研究.孙肇才、张渝昌主编.中国含油气盆地分析——朱夏学术思想研讨文集.北京:石油工业出版社,199347~54.
    [19]
    孙肇才,邱蕴玉,郭正吾.板内形变与晚期次生成藏——扬子区海相油气总体形成规律的探讨.石油实验地质,1991,13(2):107~142.
    [20]
    Allen P A and Allen J R.Basin analysis:principles and applica-tions.Oxford:Black well,1992.
    [21]
    Parnell J(ed.).Basins on the A tlantic seaboard,petroleum geology,sedimentology and basin evolution.Geological Society Special Publication 62,1992.
    [22]
    Lin Changsong,Zhang Yanmei,Li Sitian and Zhang Qiming.Sequence stratigraphy modelling of sedimentary basins:application to Erlian and Yinggehai basins in China.Journal of China University of Geosciences,1996,7:132~137.
    [23]
    Weimer R J.Sequence stratigraphic concepts applied to integrated oil and gas field development with case histories.1993~1994 AAPG Distinguished Lectures.
    [24]
    朱夏.活动论构造历史观.石油实验地质,1991,13(3):201~209.
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