南沙曾母盆地与北巴拉望盆地碳酸盐台地形成演化及其比较沉积学
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摘要
勘探证实,生物礁—碳酸盐岩是南沙沉积盆地油气勘探主要目的层系,因此,相关研究具有重要的理论实际意义。根据来自该区有关三维地震、钻井岩心精细分析的资料,对南沙上第三系曾母盆地路科尼亚(Luconia)及北巴拉望盆地马拉帕亚(Malampaya)生物礁—碳酸盐岩进行了对比分析,指出二者都形成于南海扩张过程中微陆块断裂、碰撞、拼接的构造背景下,由于发育时期及构造部位的差异,演化进程很不相同。路科尼亚台地始于晚渐新世—早中新世,中中新世—晚中新世期间最为繁盛,演化过程伴有多期进积、退积及台地翼部同沉积断裂导致的阵发性滑塌;台地中最明显的地震反射多与淹没事件有关。马拉帕亚碳酸盐台地发育相对较早,持续时间也较长,始于晚始新世,中中新世末台地发育终止。马拉帕亚碳酸盐台地发育高频米级潮下旋回,常以暴露面为界,而且台地发育明显受同沉积构造变形的影响。
引文
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[2]Wilson M E J.Cenozoic carbonates in Southeast Asia:implications for equatorial carbonate development[J].Sedimentary Geology,2002,147(3-4):295-428.
[3]Epting M.Sedimentology of Miocene carbonate build-ups,central Luconia,offshore Sarawak[J].BulletinPersatuan Geologic Malaysia,1980,12:17-30.
[4]Vahrenkamp V C.Miocene carbonates of Luconia Prov-ince,offshore Sarawak:implication for regional geologyand reservoir properties from strontium isotope stratig-raphy[J].Petronas Research and Technology Forum,1996.
[5]Lee T,Lawver L A.Cenozoic plate reconstruction ofSouth East Asia,South-East Asia structures and tec-tonics[J].Tectonophysics,1995,251:1 711-1 735.
[6]Hutchison C S.Geological evolution of South East Asia.Monographs on Geology and Geophysics[M].Oxford:Oxford University Press,1989.
[7]Grtsch J,Mercadier C.Integrated 3-D reservoir model-ing based on 3-D seismic:The Tertiary Malampaya andCamago buildups,offshore Palawan,Philippines[J].AAPG Bulletin,1999,83:1 703-1 727.
[8]Valentina Z,Wolfgang S,Jan-Henk van K,et al.3DSeismic characterization of submarine landslides on aMiocene carbonate platform(Lucania Province,Malay-sia)[J].Sedimentary Research,2004,74(6):817-830.
[9]Fournie F,Borgomano J,Montaggioni L F.Develop-ment patterns and controlling factors of Tertiary car-bonate buildups:Insights from high-resolution 3D seis-mic and well data in the Malampaya gas field(OffshorePalawan,Philippines)[J].Sedimentary Geology,2005,175:189-215.
[10]Schlter H U,Hinz K,Block M.Tectono-stratigraphicterranes and detachment faulting of the South China Seaand Sulu Sea[J].Marine Geology,1996,130(1/2):39-78.
[11]Neuhaus D,Borgomano J,Jauffred J C,et al.Quanti-tative seismic reservoir characterization of an OligoceneMiocene carbonate build-up,Malampaya Field,Philip-pines[C]//Eberli G,Sarg E,Massaferro J.AAPGSpecial Publication Carbonate Seismic Atlas',2003.
[12]Valentina Z,Wolfgang S,Jan-Henk van K,et al.Ar-chitecture and growth history of a Miocene carbonateplatform from 3D seismic reflection data,Luconiaprovince,offshore Sarawak,Malaysia[J].Marine andPetroleum Geology,2004,21:517-534.
[13]Fournier F,Montaggioni L,Borgomano J.Paleoenvir-onments and high-frequency cyclicity from CenozoicSouth-East Asian shallow-water carbonates:a casestudy from the Oligo-Miocene buildups of Malampaya(Offshore Palawan,Philippines)[J].Marine and Pe-troleum Geology,2004,21:1-21.
[14]Boss S K,Rasmunssen K A.Misuse of Fischer plots assealevel curves[J].Geology,1995,23(3):221-224.
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