油气勘探

四川盆地震旦系气源特征与原生含气系统有效性

  • 赵文智 ,
  • 谢增业 ,
  • 王晓梅 ,
  • 沈安江 ,
  • 魏国齐 ,
  • 汪泽成 ,
  • 王坤
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  • 1.中国石油勘探开发研究院,北京 100083;
    2.中国石油大学(北京)地球科学学院,北京 102249;
    3.中国石油天然气集团有限公司天然气成藏与开发重点实验室,河北廊坊 065007;
    4.中国石油杭州地质研究院,杭州 310023
赵文智(1958-),男,河北昌黎人,博士,中国石油勘探开发研究院教授级高级工程师,中国工程院院士,主要从事石油天然气地质综合研究和科研管理工作。地址:北京市海淀区学院路20号,中国石油勘探开发研究院,邮政编码:100083。E-mail: zwz@petrochina.com.cn

收稿日期: 2021-06-10

  修回日期: 2021-09-08

  网络出版日期: 2021-11-25

基金资助

中国科学院战略性先导科技专项(A类)(XDA14010403); 国家科技重大专项(2016ZX05004,2016ZX05007-003); 中国石油天然气股份有限公司科学研究与技术开发项目(kt2020-01-03); 中国石油天然气股份有限公司科技项目“大气田(区)成藏规律与勘探关键技术研究(2021DJ0604)”

Sinian gas sources and effectiveness of primary gas-bearing system in Sichuan Basin, SW China

  • ZHAO Wenzhi ,
  • XIE Zengye ,
  • WANG Xiaomei ,
  • SHEN Anjiang ,
  • WEI Guoqi ,
  • WANG Zecheng ,
  • WANG Kun
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  • 1. Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China;
    2. College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China;
    3. Key Laboratory of Gas Reservoir Formation and Development, CNPC, Langfang 065007, China;
    4. Hangzhou Research Institute of Geology (HIPG), PetroChina, Hangzhou 310023, China

Received date: 2021-06-10

  Revised date: 2021-09-08

  Online published: 2021-11-25

摘要

基于震旦系和寒武系烃源岩地球化学特征及与已发现气藏对比关系,辅以成藏条件分析,探讨震旦系天然气来源,明确了震旦系烃源岩的成藏贡献及原生含气系统有效性。通过天然气组成、碳氢同位素及震旦系成藏组合有效性分析,认为:①震旦系原生天然气具有低乙烷含量、重乙烷碳同位素组成和轻甲烷氢同位素组成3个特点,明显不同于寒武系;②震旦系气藏是震旦系与寒武系双源形成的混源气藏,震旦系贡献比例在灯影组四段与灯影组二段不同,位于灯影组四段台缘带和台内的贡献比分别为39%和55%,位于灯影组二段台缘带和台内的贡献比分别为54%和68%;③震旦系原生含气系统的有效性取决于源灶生气有效性、储集层有效性与成藏要素组合有效性。高过成熟海相层系天然气来源除液态烃热裂解成气外,Ro<3.5%的区域,烃源岩干酪根仍具有一定的热降解生气潜力。震旦系微生物白云岩在深层环境仍发育规模优质储集层,且在川中古隆起范围内与其他成藏要素形成时空匹配,增加了震旦系原生含气系统存在的可能性。研究成果证实震旦系原生含气系统具有规模成藏的现实性。图6参53

本文引用格式

赵文智 , 谢增业 , 王晓梅 , 沈安江 , 魏国齐 , 汪泽成 , 王坤 . 四川盆地震旦系气源特征与原生含气系统有效性[J]. 石油勘探与开发, 2021 , 48(6) : 1089 -1099 . DOI: 10.11698/PED.2021.06.02

Abstract

Based on correlation between geochemical characteristics of Sinian and Cambrian source rocks and discovered gas reservoirs, and the analysis on geological conditions of reservoir formation, the sources of natural gas in the Sinian of Sichuan Basin have been discussed to sort out the contribution of Sinian source rocks to the gas reservoirs and effectiveness of Sinian primary gas-bearing system. Through the analysis of natural gas composition, carbon and hydrogen isotopes and effectiveness of Sinian accumulation assemblages, it is concluded that: (1) The natural gas derived from the Sinian source rock is characterized by low ethane content, heavy ethane carbon isotope and light methane hydrogen isotope, and obviously different from the gas generated by the Cambrian source rock. (2) The gas reservoirs discovered in Sinian Dengying Formation are sourced by Sinian and Cambrian source rocks, and the Sinian source rock contributes different proportions to the gas in the 4th member and the 2nd member of the Dengying Formation, specifically, 39% and 55% to the 4th member in marginal zone and intra-platform, 54% and 68% to the 2th member in the marginal zone and intra-platform respectively. (3) The effectiveness of the Sinian primary gas-bearing system depends on the gas generating effectiveness of the source kitchen, reservoir and combination of gas accumulation elements. For high-over mature marine source rocks at the Ro of less than 3.5%, besides gas generated from the thermal cracking of liquid hydrocarbon, the kerogen still has some gas generation potential by thermal degradation. In addition, the Sinian microbial dolomite still preserves relatively good-quality reservoirs despite large burial depths, which match well with other basic conditions for gas accumulation in central Sichuan paleo-uplift, increasing the possibility of Sinian primary gas-bearing system. The research results confirm that the Sinian primary gas-bearing system is likely to form large-scale accumulation.

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