首页 | 本学科首页   官方微博 | 高级检索  
     检索      

南海北部天然气水合物气源系统与成藏模式
引用本文:何家雄,卢振权,苏丕波,张伟,冯俊熙.南海北部天然气水合物气源系统与成藏模式[J].西南石油大学学报(自然科学版),2016,38(6):8-24.
作者姓名:何家雄  卢振权  苏丕波  张伟  冯俊熙
作者单位:1. 中国科学院边缘海地质重点实验室, 广东 广州 510640;2. 中国地质调查局油气资源调查中心, 北京 西城 100292;3. 国土资源部广州海洋地质调查局, 广东 广州 510760
基金项目:国家自然科学基金(41176052);国家重点基础研究发展计划(2009CB219501)。
摘    要:天然气水合物成矿成藏条件与油气成藏条件虽然存在差异,但亦存在共同之处,即均需要有充足烃源供给及烃源供给系统输送与有利聚集场所的时空耦合配置。为了深入研究天然气水合物与常规油气运聚成藏条件之差异,根据南海北部陆坡深水区构造沉积演化特点及油气地质条件与多年来油气及水合物勘探成果,综合剖析了油气及天然气水合物气源构成特点与流体运聚输导系统特征,同时根据地质地球物理及地球化学分析,初步研究了气源供给运聚通道系统类型与高压低温天然气水合物稳定带的时空耦合配置关系,并结合油气地质及天然气水合物成矿成藏基本地质条件,总结和建立了南海北部陆坡深水区“生物气源自生自储扩散运聚型”、“热解气源断层裂隙输导下生上储运移渗漏型”和“热解气源底辟及气烟囱输导下生上储运移渗漏型”等3种成因类型的天然气水合物成矿成藏模式,以期能为南海北部深水区天然气水合物资源预测及有利勘查目标评价优选等提供决策依据与指导。

关 键 词:南海北部深水区  天然气水合物气源  高压低温水合物稳定带  成矿成藏模式  主控因素  
收稿时间:2016-09-03

Source Supply System and Reservoir Forming Model Prediction of Natural Gas Hydrate in the Deep Water Area of the Northern South China Sea
HE Jiaxiong,LU Zhenquan,SU Pibo,ZHANG Wei,FENG Junxi.Source Supply System and Reservoir Forming Model Prediction of Natural Gas Hydrate in the Deep Water Area of the Northern South China Sea[J].Journal of Southwest Petroleum University(Seience & Technology Edition),2016,38(6):8-24.
Authors:HE Jiaxiong  LU Zhenquan  SU Pibo  ZHANG Wei  FENG Junxi
Institution:1. CAS Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou, Guangdong 510640, China;2. Oil and Gas Survey, China Geological Survey, Xicheng, Beijing 100029, China;3. Guangzhou Marine Geology Survey, Ministry of Land and Resource, Guangzhou, Guangdong 510760, China
Abstract:Although differences exist in formation conditions between natural gas hydrate reservoirs and petroleum accumulation, they also have some requirements in common. Both of them need the spatiotemporal coupling configuration between sufficient hydrocarbon source supply, source supply transportation system and favorable gathering places. In order to further study the differences in formation conditions, this paper deeply analyzes the gas sources composition of petroleum and gas hydrate, and the characteristics of fluid migration transporting system, based on the tectonic sedimentary evolution, petroleum geological conditions, and oil, gas and gas hydrate exploration results of the northern South China Sea continental slope areas in the past. In addition, according to the analysis results of geology, geophysics and geochemistry, the space-time coupling configuration relationship between the types of gas migration channel system and the gas hydrate stability zone characterized by high pressure and low temperature are also dissected synthetically. Based on the basic geological conditions of oil/gas and gas hydrate reservoir, three models of natural gas hydrate formation and accumulation in northern slope deep-water area of South China Sea are summarized and established, "biogenic gas accumulated in place by way of self-generation and self-bearing", "thermal gas accumulated offsite through faults and fractures by way of lower-generation and upper storage", and "thermal gas accumulated offsite through mud diapir and gas chimney by way of lower-generation and upper storage". This paper hopes to provide decision-making basis and guidance for the prediction of natural gas hydrate resources and the favorable exploration target evaluation in the deep water area of the northern South China Sea.
Keywords:deepwater area of northern South China Sea  gas sources of gas hydrate  gas hydrate stability zone with high pressure and low temperature  mineralization and accumulation model  main controlling factor  
本文献已被 CNKI 等数据库收录!
点击此处可从《西南石油大学学报(自然科学版)》浏览原始摘要信息
点击此处可从《西南石油大学学报(自然科学版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号