南海北部深水区新生代断裂特征与油气聚集
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摘要
为了揭示南海北部深水区新生代断裂构造特征及其与油气聚集的关系,以地震资料解释为基础结合钻测井资料,通过编制构造几何学图件,运用油区构造解析原理,对南海北部深水区新生代断裂特征及其发育演化进行系统分析。该区主要发育东西,北东—南西,北东东—南东东3个走向的断裂;北东和北东东走向的断裂形成时间早于近东西走向的断裂。以珠江组—三亚组为界,南海北部深水区形成了基底和盖层上下两套断裂系统,主要发育持续型、中衰型和晚生型3种类型的正断层,形成了伸展、走滑和垂直3种构造样式。断裂活动控制了南海北部烃源岩的演化与分布、圈闭形成以及油气的运聚;断陷期是主要的烃源岩形成期,持续沉降有利于烃源岩保存和成熟;强烈的构造活动形成了多种类型的圈闭,其中在古近系和早中新统时期断裂发育密集,形成众多与断裂和背斜有关的构造圈闭。根据断裂发育和演化特征,由于持续性基底断裂的长期活动,在缓坡带和盆地中的坳中隆和凸起等构造高部位是油气聚集的有利场所,也是深水区下一步油气勘探的重要方向。
To reveal the relationship between the Cenozoic fault structure and the hydrocarbon in the deepwater area of northern South China Sea,based on seismic data interpretation and drill logging data to system analysis fault characteristics and development evolution,by making structural geometry datum,use oil region structure analysis principle.Development of three main trend fault(EW,NE-SW,NEE-SWW),which trend of EW development later than trend of NE-SW and NEE-SWW,to the Zhujiang-Sanya formation as boundaries of basement and cover fault system,development long-term active,presenileactive and late-developed active three types of fault and extension,strike-slip,vertical three types of structural style.Fault activities controlled evolution and distribution of source rock,trap forming and and hydrocarbon accumulation.Faulted Period is important time for source rock,continuous subsided is helpful for its preservation and maturation.Strong tectonic movement formed various types of trap,in Paleogene and Early Miocene,dese fault formed many faults and the anticline structure trap. According to the fault development and evolution features,because the long-term continuous base faults activities,in the ramp zone and the depression of the basin of lung and tectonic uplift high part is oil and gas accumulation of favorable places,which is the next step the important direction of oil and gas exploration in the deep water area.
To reveal the relationship between the Cenozoic fault structure and the hydrocarbon in the deepwater area of northern South China Sea,based on seismic data interpretation and drill logging data to system analysis fault characteristics and development evolution,by making structural geometry datum,use oil region structure analysis principle.Development of three main trend fault(EW,NE-SW,NEE-SWW),which trend of EW development later than trend of NE-SW and NEE-SWW,to the Zhujiang-Sanya formation as boundaries of basement and cover fault system,development long-term active,presenileactive and late-developed active three types of fault and extension,strike-slip,vertical three types of structural style.Fault activities controlled evolution and distribution of source rock,trap forming and and hydrocarbon accumulation.Faulted Period is important time for source rock,continuous subsided is helpful for its preservation and maturation.Strong tectonic movement formed various types of trap,in Paleogene and Early Miocene,dese fault formed many faults and the anticline structure trap. According to the fault development and evolution features,because the long-term continuous base faults activities,in the ramp zone and the depression of the basin of lung and tectonic uplift high part is oil and gas accumulation of favorable places,which is the next step the important direction of oil and gas exploration in the deep water area.
引文
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何家雄,陈胜红,刘海龄,刘士林.2009.珠江口盆地白云凹陷北坡—番禺低隆起天然气成因类型及其烃源探讨.石油学报,30(1):16-21. He Jiaxiong,Chen Shenghong,Liu Hailing and Liu Shilin.2009.Natural gas genetic types and source rocks in the northern slope of Baiyun sag to Panyu low uplift in Pearl River Mouth Basin.Acta Petrolei Sinica,30(1 ):16-21.
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何书,杨桥,漆家福,王家鼎.2008.黄骅坳陷中区新生代断裂系统及其成因分析.地质科学,43(3):533-545. He Shu,Yang Qiao,Qi Jiafu and Wang Jiading.2008.Cenozoic fault systems and their genetic analysis in central area of the Huanghua depression.Chinese Journal of Geology,43(3):533-545.
刘正华,陈红汉.2011.琼东南盆地东部地区油气形成期次和时期.现代地质,25(2):279-288. Liu Zhenghua and Chen Honghan.2011.Hydrocarbon charging orders and times in the eastern area of Qiongdongnan Basin. Geoscience,25(2):279-288.
李大伟,李德生,陈长民,黄慧鹏.2007.深海扇油气勘探综述.中国海上油气,19(1):18-24. Li Dawei,Li Desheng,Chen Changmin and Huang Huipeng.2007.An overview of hydrocarbon exploration in deep submarine fans.China Offshore Oil and Gast19(1 ):18-24.
李友川,邓运华,张功成,傅宁,孙玉梅.2011a.南海北部第三系海相烃源岩.石油学报,32(2):221-225. Li Youchuan,Deng Yunhua,Zhang Gongcheng,Fu Ning and Sun Yumei.2011a.Tertiary marine source rocks in the northern South China Sea.Acta Petrolei Sinica,32(2):221-225.
李友川,米立军,张功成,傅宁,孙玉梅.2011b.南海北部深水区烃源岩形成和分布研究.沉积学报,29(5):970- 979. Li Youchuan,Mi Lijun,Zhang Gongcheng.Fu Ning and Sun Yumei.2011b.The formation and distribution of source rocks for deep water area in the northern of South China Sea.Acta Sedimentologica Sinica,29(5):970-979.
林闻,周应金.2009.世界深水油气勘探新进展与南海北部深水油气勘探.石油物探,48(6):601-605. Lin Wen and Zhou Yingjin.2009.Progress of deepwaler hydrocarbon exploration worldwide and the exploration in the deepwater region of northern South China Sea.Geophysical Prospecting for Petroleum,48(6):601-605.
雷超,任建业,裴健翔,林海涛,尹新义,佟殿君.2011.琼东南盆地深水区构造格局和幕式演化过程.地球科学,36 (1):151-162. Lei Chao,Ren Jianye,Pei Jianxiang,Lin Haitao,Yin Xinyi and Tong Dianjun.2011.Tectonic framework and multiple episode tectonic evolution in deepwater area of Qiongdongnan Basin,northern continental marlin of South China Sea.Earth Science,36(1):151 - 162.
能源,吴景富,漆家福,张功成,何玉平,苏克露,廖晶.2011.琼东南——珠江口盆地深水区构造样式及其分布特征.天然气工业,31(8):32-37. Neng Yuan,Wu Jingfu,Qi Jiafu,Zhang Gongcheng,He Yuping,Su Kelu and Liao Jing.2011.Structural styles and distribution features in the deep water of the Pearl River Mouth and Qiongdongnan Basin.Natural Gas Industry,31(8):32-37.
孙杰,詹文欢,丘学林.2011.珠江口盆地白云凹陷构造演化与油气系统的关系.海洋地质与第四季地质,31(1): 101-107. Sun Jie,Zhan Wenhuan and Qiu Xuelin.2011.Relationship between tectonic evolution and pertroleum systems in Baiyun sag Pearl River Mouth Basin.Marine Geology and Quaternary Geology,31(1):101-107.
王春修.2002.国外深水油气勘探动态及经验.中国海上油气(地质),16(2):141-145. Wang Chunxiu.2002.Petroleum exploration situation and experiences in overseas deep water.China Offshore Oil and Gas (Geology),16(2):141-145.
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