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下刚果盆地重力滑脱构造发育特征及演化规律

, PP. 197-203

Keywords: 下刚果盆地,重力滑脱构造,构造发育,构造演化

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Abstract:

论述了西非被动大陆边缘下刚果盆地重力滑脱构造的发育特征及演化规律。下刚果盆地早白垩世至今的被动大陆边缘阶段主要发育重力滑脱构造,可分为上陆坡的重力滑脱伸展构造、中陆坡和下陆坡的重力滑脱底辟构造、下陆坡-深海平原转换区的重力滑脱冲断构造。一期完整的重力滑脱构造演化模式为从早到晚由陆向海逐渐发育的前展式发育模式,即最早发育高部位的重力滑脱伸展构造、其次发育中部的重力滑脱底辟构造、最后发育低部位的重力滑脱冲断构造。下刚果盆地总共发育两期重力滑脱构造,分别是早白垩世阿尔布期(Albian)-渐新世的第一期(早期)重力滑脱构造,中新世至今的第二期(晚期)重力滑脱构造。这两期重力滑脱构造之间呈现出从早到晚由陆向海发育的前展式结构,即晚期的重力滑脱构造位于早期重力滑脱构造的向海一侧。

References

[1]  吕福亮,贺训云,武金云,孙国忠,王根海. 2007. 安哥拉下刚果盆地吉拉索尔深水油田. 海相油气地质报, 12(1): 37-42.
[2]  马君,刘剑平,潘校华,王训练,万仑坤,刘权. 2008. 西非被动大陆边缘构造演化特征及动力学背景.中国石油勘探,(3): 60-64.
[3]  马杏垣. 1989. 重力作用与构造运动.北京:地质出版社: 1-19.
[4]  马杏垣,索书田. 1984.论滑脱及岩石圈内多层次滑脱构造. 地质学报,(3): 205-213.
[5]  彭美丽,易金,姚蓉,吴川,朱江建,王岳军,孙珍,林舸.2011.华南多层推滑构造系的物理模拟实验. 大地构造与成矿学,35(2):198-206.
[6]  索书田. 1983. 重力滑动构造. 武汉地质学院学报,(3): 11-22.
[7]  王月然,魏红兴,蒋荣敏,黄少英.2009.库车坳陷中段盐相关构造形成控制因素. 大地构造与成矿学,33(1):66-75.
[8]  余一欣,周心怀,彭文绪,魏刚,吕丁友.2011.盐构造研究进展述评. 大地构造与成矿学,35(2):169-182.
[9]  张树林,邓运华. 2009. 下刚果盆地油气勘探策略. 海洋地质动态,25(9):24-29.
[10]  Anka Z, Seranne M and Primio R. 2010. Evidence of a large upper-Cretaceous depocentre across the Continent-Ocean boundary of the Congo-Angola basin. Implications for palaeo-drainage and potential ultra-deep source rocks. Marine and Petroleum Geology, 27(3): 601-611.
[11]  Costa J L D, Schirmer T W and Laws B R. 2000. Lower Congo basin, deep-water exploration province, offshore west Africa. AAPG, 1: 12-15.
[12]  Coward M P, Purdy E G, Ries A C and Smith D G. 1999.The distribution of petroleum reserves in basins of the South Atlantic margins // Cameron N R, Bate R H and Clure V S. The oil and gas habitats of the South Atlantic. Geological Society of London Special Publication, 153: 101-151.
[13]  Cramez C and Jackson M P A. 2000. Superposed deformation straddling the continental-oceanic transition in deep-water Angola. Marine and Petroleum Geology, 17(10): 1095-1109.
[14]  Fort X, Brun J P and Chauvel F. 2004. Salt tectonics on the Angolan margin, synsedimentary deformation processes. AAPG Bulletin, 88(11):1523-1544.
[15]  Giresse P. 2005. Mesozoic-Cenozoic history of the Congo Basin. Journal of African Earth Sciences, 43(1-3):301-315.
[16]  Gottschalk R R. 2002. The Lower Congo Basin, deep-water Congo and Angola: A kinematically linked extensional/ contractional system. AAPG Annual Meeting Expanded Abstracts, 3: 66.
[17]  邓荣敬,邓运华,于水,侯读杰. 2008.西非海岸盆地群油气勘探成果及勘探潜力分析. 海洋石油,28(3):11-18.
[18]  胡望水,李涛,于水,吴婵,何瑶瑶,龙小军. 2012. 西非被动大陆边缘重力滑脱构造发育演化及成因机制. 大地构造与成矿学,36(2):186-196.
[19]  胡望水,薛天庆. 1997. 底辟构造成因类型. 江汉石油学院学报,19(4):1-7.
[20]  贾承造,赵文智,魏国齐. 2003.盐构造与油气勘探. 石油勘探与开发, 30(2): 17-19.
[21]  李莉,吴慕宁,李大荣. 2005. 加蓬含盐盆地及领区油气勘探现状和前景. 中国石油勘探,(3): 57-68.
[22]  Anka Z, Seranne M, Lopez M, Scheck-Wenderoth M and Savoye B. 2009. The long-term evolution of the Congo deep-sea fan: A basin-wide view of the interaction between a giant submarine fan and a mature passive margin(ZaiAngo project). Tectonophysics, 470(1-2): 42?56.
[23]  Arthur T J, Macgregor D S and Cameron N R. 2003. Petroleum geology of Africa: New themes and developing technologies. Published by The Geological Society London: 61-85.
[24]  Broucke O, Temple F, Rouby D, Robin C, Calassou S, Nalpas T and Guillocheau F. 2004. The role of deformation processes on the geometry of mud-dominated turbiditic systems, Oligocene and Lower-Middle Miocene of the Lower Congo basin(West African Margin). Marine and Petroleum Geology, 21(3): 327-348.
[25]  Brun J P and Fort X. 2004. Compressional salt tectonics(Angolan margin). Tectonophysics, 382(3-4): 129-150.
[26]  Guiraud M and Buta-Neto.2010. Segmentation and differential post-rift uplift at the Angola margin as recorded by the transform-rifted Benguela and oblique-to-orthogonal-rifted, Kwanza basins. Marine and Petroleum Geology, 27(5): 1040?1068. Jackson M P A, Hudec M R, Jennette D C and Kilby R E. 2008. Evolution of the Cretaceous Astrid thrust belt in the ultradeep-water Lower Congo Basin, Gabon. AAPG Bulletin, 92(4):487?511.
[27]  Lavier L L and Steckler M S. 2000. An improved method for reconstructing the stratigraphy and bathymetry of continental margins: Application to the Cenozoic tectonic and sedimentary history of the Congo margin. AAPG Bulletin, 84,(7): 923-939.
[28]  Marton L G, Tari G C and Lehmann C T.2000. Evolution of the Angolan passive margin, West Africa, with emphasis on post-salt structural styles // Webster M and Talwani M. Atlantic Rifts and Continental Margins. American Geophysical Union, Geophysical Monograph Series, 115:129-149.
[29]  Rowan M G, Peel F J and Vendeville B C. 2004. Gravity- driven fold belts on passive margins // McClay K R. Thrust tectonics and hydrocarbon systems. AAPG Memoir, 82: 157-182.
[30]  Savoye B and Babonneau N. 2009. Geological overview of the Angola-Congo margin, the Congo deep-sea fan and its submarine valleys. Deep-Sea Research II,56(23):2169-2182.
[31]  Spathopoulos F.1996.An insight on salt tectonics in the Angola Basin, South Atlantic // Blundel D J, Alsop G I and Davison J. Salt tectonics. Geological Society(London)Special Publication, 100: 153-174.
[32]  Tari G, Molnar J and Ashton P. 2003.Examples of salt tectonics from West Africa: A comparative approach. Petroleum geology of Africa: New Themes and Developing Technologies. Geological Society, London, Special Publications, 207: 85-104.

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