收稿日期: 2006-12-20
修回日期: 2007-04-18
网络出版日期: 2007-06-10
基金资助
国家自然科学基金重点项目“南海深水扇系统及油气资源”（编号：40238060）；国家自然科学基金项目“白云凹陷成盆机理的数学模拟研究”（编号：40576027）共同资助.
Tectonic Features of World's Major Deep-water Oil/Gas Fields and Their Enlightenment to Deep-water Exploration in Northern South China Sea
Received date: 2006-12-20
Revised date: 2007-04-18
Online published: 2007-06-10
介绍世界著名深水油气盆地的主要特征，着重构造特征，并与南海北部深水区进行了对比。世界著名深水油气盆地产出的大地构造条件具多样性，虽然大多数位于开阔大洋被动陆缘（南大西洋裂谷系、北海、澳大利亚西北陆架盆地），但边缘海的被动陆缘（墨西哥湾盆地）、转换大陆边缘（洛杉矶盆地）、主动陆缘（南沙海槽盆地）也可形成极佳的深水含油气盆地。南海北部深水区具有世界某些重要深水含油气盆地类似的特征，如位于被动陆缘和大河出口下方，以裂陷期的湖相富有机质页岩为主要生油岩，白云凹陷发育上下叠置的6层深水扇等，这都是有利的石油地质条件。但南海北部深水区盐层和盐构造不发育，构造圈闭相对较不发育，使深水油气系统的研究更加困难，也更具开拓意义。
周蒂 , 陈汉宗 , 孙珍 . 世界著名深水油气盆地的构造特征及对我国南海北部深水油气勘探的启示[J]. 地球科学进展, 2007 , 22(6) : 561 -572 . DOI: 10.11867/j.issn.1001-8166.2007.06.0561
Major features, especially tectonic features of world's famous deep-water oil/gas fileds are outlined, which demonstrated the structural diversity of hydrocarbon accumulation in deep-water environment. Although majority of giant fields are discovered in the passive continental margins of open oceans (e.g. the South Atlantic rift system, the North Sea, the NW Australia shelf), giant and large fields have been found also in the passive continental margins of marginal seas (e.g. the Gulf of Mexico), transfer continental margins (e.g. the Los Angeles basin), and active convergent margins (e.g. the NW Borneo trough). In comparison, the deep-water region of northern South China Sea shares some favorite features with respective world's famous deep-water fields, such as being located in passive continental margin and feed by a major river system, having organic-rich lacustrine shale as major source rocks, having overlapped layers of deep-water fans,etc. On the other hand, in the deep-water region of northern South China Sea no salt and salt tectonics, and structural traps are less developed. These put forward new challenge to the hydrocarbon exploration in deep-water northern South China Sea.
[1]Wilson M, Guiraud R. Magmatism and rifting in Western and Central Africa, from Late Jurassic to recent times［J］.Tectonophysics, 1992, 213: 203-225.
[2]Maurin J C, Guiraud R. Basement control in the development of the early cretaceous west and central African rift system［J］.Tectonophysics, 1993, 238: 81-95.
[3]Peate D W. The Paraná-Etendeka province[C]//Mahoney J J, Coffin M F, eds. Large Igneous Provinces American Geophysical Union Geophysical Monograph. 1997,100: 217-245.
[4]Filho P A P, Santos F L S G, Mansoori A. An update on the developments in petroleum production research in Brazil［J］.Journal of Petroleum Science and Engineering, 2006, 51: 1-5.
[5]Chang H K, Kowsmann R O, Figueiredo A M F,et al. Tectonics and stratigraphy of the East Brazil rift system: An overview［J］.Tectonophysics, 1992, 213: 97-138.
[6]Guardado L R, Gamboa L A P, Lucchesi C F. Petroleum geology of the Campos basin, Brazil:A model for a producing Atlantic-type basin[C]//Edwards, Santogrossi, eds. Divergent/Passive Margin Basins:AAPG Memoir 48,1990:3-79.
[7]Meisling K E, Cobbold P R, Mount V S. Segmentation of an obliquely rifted margin, Campos and Santos basins, southeastern Brazil［J］.AAPG Bulletin,2001，85（11）:1 903-1 924.
[8]Viana A F, Faugères A, Lima J C,et al. The Sao Tomé deep-sea turbidite system (southern Brazil Basin): Cenozoic seismic stratigraphy and sedimentary processes［J］.AAPG Bulletin,2003, 87(5): 873-894.
[9]Demercian S, Szatmari P, Cobbold P R. Style and pattern of salt diapirs due to thin-skinned gravitational gliding, Campos and Santos basins, offshore Brazil[J］.Tectonophysics,1993, 228(3/4): 393-422.
[10]Ala M A, Selley R C. The west African coastal basins[C]//Selley R C, ed. African Basins. Amsterdam: Elsevier Science, 1997:173-186.
[11]Valle P J, Gjelberg J G, Helland-Hanse W. Tectonostratigraphic development in the eastern lower Congo Basin, offshore Angola, West Africa［J］.Marine and Petroleum Geology, 2001, 18(8): 909-927.
[12]Jackson M P A, Talbot C J. A Glossary of Salt Tectonics［M］. Austin:University of Texas, 1991.
[13]Harris N B, Freeman K H, Pancost R D,et al. The character and origin of lacustrine source rocks in the Lower Cretaceous synrift section, Congo Basin, west Africa［J］.AAPG Bulletin, 2004, 88(8): 1 163-1 184.
[14]Anderson J E, Cartwright J, Drysdall S J,et al. Controls on turbidite sand deposition during gravity-driven extension of a passive margin: Examples from Miocene sediments in Block 4, Angola［J］.Marine and Petroleum Geology, 2000, 17(10): 1 165-1 203.
[15]Heini P I, Davies R J. Degradation of compressional fold belts: Deep-water Niger Delta［J］.AAPG Bulletin, 2006, 90(5): 753-770.
[16]Doust H, Omatsola E. Nigeria delta[C]//Edwards, Santogrossi, eds. Divergent/Passive Margin Basins: AAPG Memoir 48, 1990:201-238.
[17]Corredor F, Shaw J H, Bilotti F. Structural styles in the deep-water fold and thrust belts of the Niger delta［J］.AAPG Bulletin, 2005, 89(6): 753-780.
[18]Wu S, Bally A W. Slope tectonics-Comparisons and contrasts of structural styles of salt and shale tectonics of the northern Gulf of Mexico with shale tectonics of offshore Nigeria in Gulf of Guinea[C]//Mohriak W, Talwani M, eds. Atlantic Rifts and Continental Margins. Washington DC:American Geophysical Union, 2000:151-172.
[19]Bird D E, Burke K, Hall S A,et al.Gulf of Mexico tectonic history: Hotspot tracks, crustal boundaries, and early salt distribution［J］.AAPG Bulletin, 2005, 89(3): 311-328.
[20]Stover S C, Ge S, Weimer P,et al. The effects of salt evolution, structural development, and fault propagation on Late Mesozoic-Cenozoic oil migration: A two-dimensional fluid-flow study along a megaregional profile in the northern gulf of Mexico basin［J］.AAPG Bulletin, 2001, 85(11): 1 945-1 966.
[21]Weimer P, Rowan M G,McBride B C,et al. Evaluating the petroleum systems of the northern deep gulf of Mexico through integrated basin analysis: An overview［J］.AAPG Bulletin, 1998, 82(5B): 865-877.
[22]Grando G, McClay K. Structural evolution of the Frampton growth fold system, Atwater Valley-Southern Green Canyon area, deep water gulf of Mexico［J］.Marine and Petroleum Geology, 2004, 21: 889-910.
[23]Biddle K T. The Los Angeles Basin: An overview[C]//Biddle K T, eds. Active Margin Basins. Tulsa: American Association of Petroleum Geologists, 1991:5-24.
[24]Redin T. Oil and gas production from submarine fans of the Los Angeles Basin[C]//Biddle K T, eds. Active Margin Basins:AAPG Memoir 52,1991:239-259.
[25]Allman W P, Tromp J P, Abdullah I. Tectonostratigraphic controls on turbidite depositional processes in Brunei［J］.AAPG Bulletin, 2000, 84(9): 1 397.
[26]Ingram G M, Chisholm T J, Grant C J,et al. Deepwater North West Borneo: Hydrocarbon accumulation in an active fold and thrust belt［J］.Marine and Petroleum Geology,2004, 21: 879-887.
[27]Zhou Di, Wu Shimin, Chen Hanzong.Some remarks on the tectonic evolution of Nansha and its adjacent regions in South China Sea[J].Geotectonica et Metallogenica,2005,29(3): 339-345. [周蒂, 吴世敏，陈汉宗. 南沙海区及邻区构造演化动力学的若干问题［J］. 大地构造与成矿学, 2005, 29(3): 339-345.]
[28]Crevello P. Turbidite and deepwater depositional systems of Borneo; foredeep slope and basin floor fan systems［J］.AAPG Bulletin,2001, 85(4): 762.
[29]Anuar A, Muhamad A J. Case study on source rock deposition and preservation; NW Borneo deep water areas［J］.AAPG Bulletin, 2000, 84(9): 1 398.
[30]Pang Xiong, Yang Shaokun, Zhu Ming,et al. The deep-water fan systems and petroleum resource in the northern slope of south China Sea[J].Acta Geologica Sinica, 2004, 78(3): 626-631.
[31]Huang Chunju, Zhou Di, Sun Zhen,et al. Deep crustal structure of Beiyun Sag, northern South China Sea revealed from deep seismic reflection profile[J].Chinese Science Bulletin,2005, 50(11): 1 131-1 138.
[32]Sun Zhen, Pang Xiong, Zhong Zhihong,et al. Dynamics of Cenozoic tectonic evolution of the Baiyun Sag, Zhujiangkou Basin[J].Earth Science Frontiers,2005, 12(4): 489-498. [孙珍，庞雄，钟志洪，等. 珠江口盆地白云凹陷新生代构造演化动力学[J].地学前缘，2005，12(4): 489-498.]
[33]Pang Xiong, Chen Changmin, Shi Hesheng,et al. Relative sealevel changes and its response in the Zhujiang deep-water fan system, South China sea[J].Earth Science Frontiers,2005, 12(3): 167-177. [庞雄, 陈长民, 施和生, 等. 相对海平面变化与南海珠江深水扇系统的响应［J］. 地学前缘, 2005, 12(3): 167-177.]
/
| 〈 |
|
〉 |
甘公网安备62010202000687
