天然气地球科学 ›› 2011, Vol. 22 ›› Issue (6): 935–942.doi: 10.11764/j.issn.1672-1926.2011.06.935

• 天然气地质学 •    下一篇

南海北部边缘盆地不同类型非生物成因CO2成因成藏机制及控制因素

 何家雄, 祝有海, 黄霞, 龚晓峰   

  1. 1.中国科学院边缘海地质重点实验室,广东 广州 510640;
    2.中国地质科学院矿产资源研究所,北京 100037
  • 收稿日期:2011-08-02 修回日期:2011-12-06 出版日期:2011-12-10 发布日期:2011-12-10
  • 通讯作者: 何家雄hejx@gig.ac.cn. E-mail:hejx@gig.ac.cn.
  • 作者简介:何家雄(1956-),男,湖北天门人,研究员,博士,主要从事南海油气勘探与油气地质研究.E-mail:hejx@gig.ac.cn.
  • 基金资助:

    国家重点基础研究发展计划项目(编号:2009CB219501)联合资助.

Accumulated Mechanisms for Different Genetic Types of Non-biological CO2 and Controlling Factors in North Marginal Basins, South China Sea

 HE  Jia-Xiong, ZHU  You-Hai, HUANG  Xia, GONG  Xiao-Feng   

  1. 1.Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou 510640, China;
    2.Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037,China .
  • Received:2011-08-02 Revised:2011-12-06 Online:2011-12-10 Published:2011-12-10

摘要:

南海北部边缘盆地非生物成因CO2资源丰富,依据通常的成因判识与划分参数(δ13CCO2和3He/4He),结合运聚成藏的具体地质条件及控制因素,可将CO2成因成藏机制明确划分为泥底辟热流体控制的壳源型及壳幔混合型CO2成因成藏机制和火山幔源活动及深大断裂输导控制的火山幔源型CO2成因成藏机制2种类型。前者,即壳源型及壳幔混合型成因CO2资源丰富储量规模大,这种成因成藏机制形成的CO2运聚成藏规律复杂,主要富集于西北部走滑伸展型边缘的莺歌海盆地中央泥底辟构造带浅层,具有平面上分区、分块、纵向上分层、分带多期运聚成藏的特点,且主要受控于泥底辟热流体上侵活动与巨厚海相含钙砂泥岩的物理化学综合作用;后者即火山幔源型成因CO2在该区资源及储量规模较小,多分布在处于北部裂陷带的琼东南盆地东部Ⅱ断裂带周缘和珠江口盆地北部深大断裂发育区,且主要受控于火山幔源岩浆脱排气之CO2气源供给与深大断裂导气输送作用的有效配置。

关键词: 南海北部边缘盆地/壳源型CO2, 火山幔源型CO2, CO2运聚成藏机制, 主要控制因素

Abstract:

There is plenty of non-biological CO2 in the north marginal basins of South China Sea. Based on patterns of gas origins and classified parameters (i.e. δ13C CO2 ,3He/4He) as well as specific geological conditions of gas migration and accumulation, two types of CO2 sources are classified into crustal-type CO2 or mixing of crust-mantle mixed type  CO2  controlled by both muddy diapiric thermal fluid, and mantle-type CO2 acted by mantle-derived volcanic activity and deep fault. The crustal-type and mixing of crust-mantle type CO2 is widely distributed. After the complex processes of migration and accumulation, this type of CO2 is mainly clustered in the shallow layer of central muddy diapirs zone in the strike-slip extensional brim of northwest Yingge Sea basin, which is characterized as partition block in plane and multi-layer and zone in vertical. So, the crustal-type and mixing of crust-mantle type CO2 accumulation is controlled by muddy diapir intrusion activity and physical-chemical combined action about thick marine calcium sand-shale. Few amount of mantle-type CO2 is developed in the Ⅱfault zone and it's surrounding of eastern Qiongdongnan basin. The mantle-type CO2 accumulation is mainly controlled by mantle-derived volcanic activity and deep fault.

Key words: North marginal basins of South China Sea, Crustal-type CO2, Mantle-type CO2, CO2 migration and accumulation mechanisms, Controlling factors.

中图分类号: 

  • TE122

[1]Gutzler D S.Evaluating global warming:A post-1990s perspective[J].GSA Today,2000,10:345-351.
[2]Wang Zhenfeng,He Jiaxiong,Pei Qiubo.The origin and migration-accumulation features of CO2 in Ying-Qiong basin and the western Pearl River mouth basin[J].China Offshore Oil and Gas:Geology,2003,17(5):293-297.[王振峰,何家雄,裴秋波.莺—琼盆地和珠江口盆地西部CO2成因及运聚分布特征[J].中国海上油气:地质,2003,17(5):293-297.]
[3]He Jiaxiong,Liu Quanwen.The analysis and discussion to the characterson generative cause,migration and distribution of CO2 in Ying-Qiong basins in the north of the South China Sea[J].Natural Gas Geoscience,2004,15(1):12-19.[何家雄,刘全稳.南海北部大陆架边缘盆地CO2成因和运聚规律的分析与预测[J].天然气地球科学,2004,15(1):12-19.]
[4]
[JP2]He Jiaxiong,Li Mingxing,Chen Weihuang.Geotemperature field and up-welling action of hot flow body and its relationship with natural gas migration and accumulation in Yinggehai basin[J].Natural Gas Geoscience,2000,11(6):29-43,Ⅲ.[何家雄,李明兴,陈伟煌.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,Ⅲ.]
[5]He Jiaxiong,Chen Weihuang,Zhong Qixiang.A investigation on shallow natural gas forming factor and hydrocarbon source for Yinggehai basin mud diapir belt[J].Natural Gas Geoscience,1994,5(6):15-27,14.[何家雄,陈伟煌,钟启祥.莺歌海盆地泥底辟带浅层天然气成因及烃源探讨[J].天然气地球科学,1994,5(6):15-27,14.]
[6]He Jiaxiong.The preliminary study of CO2 gas in Yinggehai basin[J].Natural Gas Geoscience,1995,6(6):1-12.[何家雄.莺歌海盆地CO2天然气的初步研究[J].天然气地球科学,1995,6(6):1-12.]
[7]He Jiaxiong,Zhang Wei,Chen Gang.A preliminary study on the genesis of CO2  gas and characteristics in its migration and accumulation in the Yinggehai basin[J].Petroleum Exploration and Development,1995,22 (6):8-15.[何家雄,张伟,陈刚.莺歌海盆地CO2成因及运聚特征的初步研究[J].石油勘探与开发,1995,22(6):8-15.] 
[8]Chen Gang,He Jiaxiong,Zhang Wei.The CO2 origin and the analogy of typical CO2 gas at home and abroad in Yinggehai basin[J].Natural Gas Geoscience,1996,7 (4) :1-12.[陈刚,何家雄,张伟.莺歌海盆地CO2成因及与国内外典型CO2气藏的类比[J].天然气地球科学,1996,7(4):1-12.]
[9]He Jiaxiong,Xia Bin,Liu Baoming, et al.Origin,migration and accumulation of CO2 in east China and offshore shelf basins[J].Petroleum Exploration and Development,2005,32 (4) :42-49.[何家雄,夏斌,刘宝明,等.中国东部及近海陆架盆地CO2成因及运聚规律与控制因素研究[J].石油勘探与开发,2005,32(4):42-49.]
[10]He Jiaxiong,Chen Gang.The origin of CO2 and its main source in Yinggehai basin[J].China Offshore Oil and Gas:Geology,1998,12 (3):164-167.[何家雄,陈刚,莺歌海盆地CO2成因及主气源[J].中国海上油气:地质,1998,12(3):164-167.]
[11]He Jiaxiong.Disscasion of CO2 origin in Yinggehai basin:Discuss with Mr.Huang Gaojian in China University of Geosciences[J].China Offshore Oil and Gas:Geology,2003,17(2):149-150.[何家雄.关于莺歌海盆地CO2成因问题的探讨——与中国地质大学黄高健先生商榷[J].中国海上油气:地质,2003,17(2):149-150.] 
[12]He Jiaxiong.To discuss the cause of CO2 formation in Yinggehai basin and to reply professor Chen Jianyu[J].Natural Gas Geoscience,2003,14(5):412-415.[何家雄.再论莺歌海盆地CO2成因问题——兼答陈建渝教授[J].天然气地球科学,2003,14(5):412-415.]
[13]He Jiaxiong,Chen Weihuang,Li Mingxing.Genetic types of natural gas and source rocks in Ying-Qiong basin[J].China Offshore Oil and Gas:Geology,2000,14(6):398-405.[何家雄,陈伟煌,李明兴.莺—琼盆地天然气成因类型及气源剖析[J].中国海上油气:地质,2000,14(6):398-405.]
[14]He Jiaxiong,Chen Weihuang,Li Mingxing, et al.Origin of carbon dioxide in natural gas in Ying-Qiong basin and its comprehensive gas source discrimination[J].Natural Gas Industry,2001,21(3):15-21.[何家雄,陈伟煌,李明兴,等.莺—琼盆地天然气中CO2成因及气源综合判识[J].天然气工业,2001,21(3):15-21.]
[15]He Jiaxiong,Yang Jihai,Chen Zhihong, et al.Characteristics of forming natural gas reservoirs in the medium-deep strata in Yinggehai basin[J].Natural Gas Industry,2003,23(3):15-19.[何家雄,杨计海,陈志宏,等.莺歌海盆地中深层天然气成藏特征[J].天然气工业,2003,23(3):15-19.]
[16]He Jiaxiong,Li Mingxing,Chen Shenghong.A CO2 risk analysis for mid deep gas exploration in diapir belt,Yinggehai basin[J].China Offshore Oil and Gas:Geology,2000,14 (5):332-338.[何家雄,李明兴,陈胜红.莺歌海盆地泥底辟带中深层天然气勘探中的CO2风险分析与预测[J].中国海上油气:地质,2000,14(5):332-338.]
[17]He Jiaxiong.The geological and geochemical features and origin of the gas in DongfangⅠ-Ⅰ structure of Yinggehai basin[J].Natural Gas Geoscience,1994,5(3):1-8.[何家雄.莺歌海盆地东方Ⅰ-Ⅰ构造天然气地质地化特征及成因探讨[J].天然气地球科学,1994,5(3):1-8.]
[18]He Jiaxiong,Chen Gang.The distribution,enrichment characteristics and preliminary forecast of CO2 in Yinggehai basin[J].Natural Gas Geoscience,1997,8(3):9-17.[何家雄,陈刚.莺歌海盆地CO2分布、富集特征及初步预测[J].天然气地球科学,1997,8(3):9-17.]
[19]He Jiaxiong,Chen Gang.The preliminary prediction and occurrence of CO2 in Yinggehai basin[J].Petroleum Exploration and Development,1998,25(2):20-23.[何家雄,陈刚.莺歌海盆地CO2分布及预测方法研究[J].石油勘探与开发,1998,25(2):20-23.]
[20]He Jiaxiong,Zhu Youhai,Cui Shasha, et al.Origin,migration and accumulation of CO2 and Its resource utilization in marginal basin,northern South China Sea
[J].Natural Gas Geoscience,2011,20(4):487-496.
[何家雄,祝有海,崔莎莎,等.南海北部边缘盆地CO2成因及运聚规律与资源化利用思路
[J].天然气地球科学,2011,20(4):487-496.]
[21]Teng Jiwen,Wang Guangjie,Zhang Zhongjie, et al.Three-dimensional S-wave velocity structure of the South mainland and the southern extension of the Tan-Lu fault zone[J].Chinese Science Bulletin,2000,45 (23) :2492 -3497.[滕吉文,王光杰,张中杰,等.华南大陆S波三维速度结构与郯庐断裂带的南延[J].科学通报,2000,45(23):2492-3497.] 
[22]Dai Jinxing.The CO2 gas fields (reservoir) and the gas types in eastern China and the continental shelf[J].Exploration of Nature,1996,15 (4):18-20.[戴金星.中国东部和大陆架二氧化碳气田(藏)及其气的类型[J].大自然探索,1996,15(4):18-20.]
[23]He Jiaxiong,Ma Wenhong,Chen Shenghong, et al.Non-hydrocarbon gas distribution and its geological conditions and controlling factors in the marginal basin of northern South China  Sea[J].Marine Geology and Quaternary Geology,2011,31 (2) :95-104.[何家雄,马文宏,陈胜红,等.南海北部边缘盆地非烃气分布及形成的地质条件与控制因素[J].海洋地质与第四纪地质,2011,31(2):95-104.]
[24]He Jiaxiong,Zhu Youhai,Yao Yongjian, et al.The Geology and Resource Utilization of Carbon Dioxide in the Marginal Basin of Northern South China Sea[M].Beijing:Petroleum Industry Press,2009:1-193.[何家雄,祝有海,姚永坚,等.南海北部边缘盆地二氧化碳地质及资源化利用[M].北京:石油工业出版社,2009:1-193.]

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