莺歌海盆地泥底辟成因、展布特征及其与天然气运聚成藏关系
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摘要
泥底辟是南海北部边缘西区莺歌海盆地颇具特色的地震地质异常体,具有欠压实异常、高温高压特点及低密低速的地球物理特征,其展布则具有明显分带性且沿盆地北西走向呈近南北向雁行式排列。泥底辟成因及分布,主要受控于盆地快速沉降及高速沉积充填压实与排出流体不均衡所产生的巨大异常高温高压潜能,和区域控盆断裂晚期右旋走滑伸展活动。而晚期泥底辟热流体上侵活动及其他成藏条件的有效配置,则有效地控制了天然气及CO_2运聚成藏规律。
Mud diapirs are characteristic anomalous seismic-geologic bodies in the Yinggehai basin on the northern margin of the South China Sea and have the less compact,abnormally high-pressure and -temperature and low-density and -velocity geophysical characteristics.They show pronounced zoning and are distributed en echelon in a nearly N-S direction along the northwest trend of the basin.The origin and distribution of the mud diapirs were controlled mainly by the combined action of the great abnormally high-temperature and -pressure potential energy produced by rapid subsidence of the basin and inequilibrium between the filling-compaction of rapidly deposited sediments and fluids squeezed out and the dextral strike-slip extension of regional basin-controlling faults in the late stage.The natural gas and CO_2 migration and accumulation were effectively controlled by the effective combination of the upward intrusion of the late-stage mud-diapir thermal fluids and their accumulation conditions.
Mud diapirs are characteristic anomalous seismic-geologic bodies in the Yinggehai basin on the northern margin of the South China Sea and have the less compact,abnormally high-pressure and -temperature and low-density and -velocity geophysical characteristics.They show pronounced zoning and are distributed en echelon in a nearly N-S direction along the northwest trend of the basin.The origin and distribution of the mud diapirs were controlled mainly by the combined action of the great abnormally high-temperature and -pressure potential energy produced by rapid subsidence of the basin and inequilibrium between the filling-compaction of rapidly deposited sediments and fluids squeezed out and the dextral strike-slip extension of regional basin-controlling faults in the late stage.The natural gas and CO_2 migration and accumulation were effectively controlled by the effective combination of the upward intrusion of the late-stage mud-diapir thermal fluids and their accumulation conditions.
引文
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[2] 何家雄,陈伟煌,钟启祥,等莺歌海盆地泥底辟特征及天然气勘探方向[J].石油勘探与开发,1994,21(6) :6-9． He Jiaxiong, Chen Weihuang, Zhong Qixiang, et al. Mud diapir characteristics and natural gas prospects in Yinggehai Basin [J]. Petroleum Exploration and Development, 1994,21 (6) :6-9 (in Chinese with English abstract).
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[4] 何家雄,陈红莲,陈刚,等.莺歌海盆地泥底辟带天然气成藏条件及勘探方向[J].中国海上油气(地质),1995,9(3) :155-163． He Jiaxiong, Chen Honglian, Chen Gang, et al .Gas reservoir and exploration targets of mud diapir belt,Yinggehai Basin[J].China Offshore Oil and Gas (Geology), 1995,9 (3) :157-163 (in Chinese with English abstract).
[5] 何家雄,陈伟煌,李明兴,等.莺歌海盆地热流体上侵活动与天然气运聚富集关系探讨[J].天然气地球科学,2000,11(6) :29-43． He Jiaxiong, Chen Weihuang, Li Mingxing, et al. Geotemperature field and upwelling Action of hot flow body and its relationship with natural gas migration and accumulation in Yinggehai Basin [J]. Nature Gas Geoscience, 2000,11 (6) :29-43 (in Chinese with English abstract).
[6] 何家雄,夏斌,刘宝明,等.莺歌海盆地泥底辟热流体上侵活动与天然气及CO_2运聚规律剖析[J].石油实验地质,2004,26(4) :349-358． He Jiaxiong, Xiabin, Liu Mingbao, et al. Geotemperature field and upwelling Action of hot flow body and its relationship with natural gas migration and accumulation in Yinggehai Basin [J]. Petroleum Geology and Experiment, 2004,26 (4) :349-358 (in Chinese with English abstract).
[7] 何家雄,王振峰,解习农,等.莺歌海盆地泥-流体底辟带热流体活动对天然气运聚成藏的控制作用[J].地球科学,2004,29(2) :203-210． He Jiaxiong, Wang Chenfeng, Xie Xinong, et al. Heat flow action and its control on natural gas migration and accumlation in mud-fluid diapir areas in Yinggehai Baisin [J]. Earth science, 2004,29(2) :203-210(in Chinese with English abstract).
[8] 毛云新,何家雄,张树林,等.莺歌海盆地泥底辟带昌南区热流体活动的地球物理特征及成因[J].天然气地球科学,2005,16(1) :108-113． Mao Yunxin, He Jiaxiong, Zhang Shulin, et al.Geophysical characters and origin of the thermal fluids in Changnan block of mud diapir zone in Yinggehai Basin [J]. Nature Gas Geoscience, 2005,16(1) : 108-113(in Chinese with English abstract).
[9] 郝芳,李思田,龚再升,等.莺歌海盆地底辟发育机制与流体幕式充注[J].中国科学(D辑),2001,31(6) :471-476． Hao Fang, Li Sitian, Gong Zaishen, et al. The machanics of the diapir and the fluid episodic infilling of Yinggehai Basin [J].Science in China(Ser.D),2001, 31 (6) : 471-476(in Chinese).
[10] 郝芳,邹华耀,黄保家,等.莺歌海盆地天然气生成模式及其成藏流体响应[J].中国科学(D辑),2002,32(11) :889-895． Hao Fang, Zhou Huayao, Huang Baojia, et al. Gas generation model and its responds in accumulation of nutural gas of Yinggehai Basin[J].Science in China(Ser.D), 2002,32(11) :889-895(in Chinese).
[11] 郝芳,董伟良,邹华耀,等莺歌海盆地汇聚型超压流体流动及天然气晚期快速成藏[J].石油学报,2003,24(6) :7-12． Hao Fang, Dong Weiliang, Zhou Huayao, et al. Overpressure fluid flow and rapid accumulation of natural gas in Yinggehai Basin [J]. Acta Petrolei Sinica, 2003,24 (6) :7-12 (in Chinese with English abstract).
[12] 单家增,董伟良.莺歌海盆地泥底辟构造动力学成因机制的高温高压模拟实验[J].中国海上油气(地质),1996,10(4) :209-214． Shan Jiazeng, Dong Weiliang. High temperature and high pressure modelling experiments for dynamic mechanism of the mud diapir in Yinggehai Basin [J]. China Offshore Oil and Gas (Geology),1996,10(4) :209-214(in Chinese with English abstract).
[13] 张树林,田世澄,朱芳冰,等.莺歌海盆地底辟构造的成因及石油地质意义[J].中国海上油气(地质),1996,10(1) :1-6． Zhang Shulin, Tian Shicheng, Zhu Fangbing, et al. Genesis of diapir structures in Yinggehai Basin and its significances to petroleum geology [J]. China Offshore Oil and Gas (Geology), 1996,10(1) :1-6(in Chinese with English abstract).
[14] 解习农,李思田,胡祥云,等.莺歌海盆地底辟带热流体输导系统及其成因机制[J].中国科学(D辑),1999,29(3) :247-256． Xie Xinong, Li Sitian, Hu Xiangyun, et al. Genetic mechanisms of the diapir and the fluid guide economy in Yinggehai Basin [J]. Science in China(Ser.D), 1999,29(3) :247-256(in Chinese).
[15] 李纯泉.莺歌海盆地流体底辟构造及其对天然气成藏的贡献[J].中国海上油气(地质),2000,14(4) :253-257． Li Chunquan. Fluid diapirs and their contributions to hydrocarbon accumlation in Yinggehai Basin [J]. China Offshore Oil and Gas (Geology), 2000,14(4) :253-257(in Chinese with English abstract).
[16] 黄春菊,陈开远,李思田,等.莺歌海盆地泥底辟活动期次分析[J].石油勘探与开发,2002,29(4) :44-46． Huang Chunju, Chen Kaiyuan, Li Sitian, et al. Periodicities of diapiric rise in the Yinggehai Basin [J]. Petroleum exploration and development, 2002,29(4) :44-46(in Chinese with English abstract).
[17] 张敏强,钟志洪,夏斌,等.莺歌海盆地泥-流体底辟构造成因机制与天然气运聚[J].大地构造与成矿学,2004,28(2) :118-125． Zhang Minqiang, Zhong Zhihong, Xin Bia, et al. Genetic mechanisms of mud-fluid diapir in Yinggehai Basin and hydrocarbon accumulation [J]. Geotectonica et Metallogeina.2004,28(2) : 118-125(in Chinese with English abstract).
[18] 何丽娟,熊亮萍,汪集旸,等.莺歌海盆地构造热演化模拟研究[J].中国科学,2000,30(4) :415-419． He Lijuan, Xiong Liangping, Wang Jiyang, et al. The research on thermal evolement of Yinggehai Basin [J]. Science in China(Serias D), 2000,30(4) :415-419(in Chinese).
[19] 龚再升,李思田,等南海北部大陆边缘盆地分析与油气聚集[J].北京:科学出版社,1997． 1-510． Gong Zaishen, Li Sitian, et al. The basin analysis and the accumlation of gas in the continental margin of the northern of the South Sea[M]. Beijing:Science Press, 1997． 1-510 (in Chinese with English abstract).
[20] 何家雄,昝立声,梁可明,等.莺-琼盆地泥岩压实与油气运移[J].石油勘探与开发,1991,18(增刊):34-41． He Jiaxiong, Zan Lisheng, Liang Keming, et al. Evolution of the mudrock compaction and hydrocarbon migration in Ying-Qiong Basin[J]. Petroleum Exploration and Development, 1991,18(supp.): 34-41(in Chinese with English abstract).
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