天然气地球化学

塔里木盆地阿克1气藏天然气的地球化学特征和成因

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  •  (1.中国矿业大学煤炭资源教育部重点实验室,北京 100083; 2.中国科学院广州地球化学 研究所有机地球化学国家重点实验室,广东 广州 510640; 3.中国石油塔里木油田分公 司勘探开发研究院,新疆 库尔勒 841000; 4.中国石油勘探开发研究院廊坊分院天然气 地质研究所,河北 廊坊 065007;5.美国加利福尼亚州理工学院石油能源与环境研究中心 ,美国 加利福尼亚 91789) 
李贤庆(1967-),男,浙江富阳人,教授 ,博士,现主要从事有机地球化学、油气成藏动力学与有机岩石学方面的研究工作.

收稿日期: 2004-10-08

  修回日期: 2004-12-23

  网络出版日期: 2005-02-20

基金资助

国家“十五”重点科技攻关项目(编号:2001BA605A02-0 3-01),中国博士后科学基金(编号:2002031282),国家自然科学基金(编号:40072043)联合资助.

GEOCHEMICAL CHARACTERISTICS AND ORIGIN OF NATURAL GAS FROM AKE-1 GAS POOL IN THE TARIM BASIN

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  •  (1.Key Laboratory of Coal Resources, Ministry of Education, China University of  Mining and Technology,  Beijing 100083, China; 2.The State Key Laboratory of Org anic Geochemistry, Guangzhou Institute of  Geochemistry, Chinese Academy of Scie nces, Guangzhou 510640, China; 3.The Research Institute of  Exploration and Deve lopment, Tarim Oil Field Company, CNPC, Kuerle 841000, China; 4.Institute of  Natural Gas Geology, Langfang Branch, Research Institute of Petr oleum Exploration and Development, CNPC,  Langfang 065007, China;5.The Research  Center of Petroleum Energy and Enviroment, California Institute of  Technolog y, California 91789, USA)  

Received date: 2004-10-08

  Revised date: 2004-12-23

  Online published: 2005-02-20

摘要

阿克1气藏是在塔里木盆地西南坳陷喀什凹陷油气勘探中发现的工业性气藏,这是该区天然气勘探的重大突破。根据天然气组分的含量、甲烷和乙烷碳同位素值及稀有气体同位素数据,分析了阿克1气藏天然气的地球化学特征。阿克1气藏天然气为典型干气,甲烷占优势(占80%~91%),重烃含量极低(不超过0.3%),非烃含量高(一般为20%左右),甲烷和乙烷碳同位素重(分别为-25.2‰~-24.7‰和-21.9‰~-21.1‰),稀有气体同位素比值高(3He/4He值达8.34×10-7、40Ar/36Ar值为1438)。结合地质背景,应用碳同位素动力学模拟计算结果,探讨了阿克1气藏天然气的成熟度和气源,为天然气成因评价提供了新思路。认为阿克1气藏天然气是烃源岩过成熟演化阶段的产物,其RO范围为2.0%~3.6%,属于混源气。

本文引用格式

李贤庆,肖贤明,肖中尧,胡国艺,米敬奎,唐永春, . 塔里木盆地阿克1气藏天然气的地球化学特征和成因[J]. 天然气地球科学, 2005 , 16(1) : 48 -53 . DOI: 10.11764/j.issn.1672-1926.2005.01.48

Abstract

Ake-1 is a commercial gas pool that has made great breakthrough for oil & gas e xploration in the Kashi Sag of the Southwestern Depression, Tarim Basin. On the  basis of the component content of natural gas, carbon isotope ratios of methane  and ethane, and isotope composition of rare gas, the geochemical characteristics  of Ake-1 gas pool were studied in this paper. Natural gas of Ake-1 gas pool b elongs to the typical dry gas. It has predominance methane (80%~91%), low cont ent heavy hydrocarbon (<0.3%) and high content non-hydrocarbon (generally about  20%). There are heavy carbon isotope ratios of methane (-25.2‰~-24.7‰) and e thane (-21.9‰~-21.1‰), and relatively high isotope ratios of rare gases (3He/4He 8.34×10-7, 40Ar/36Ar 1 438).  Combined with the geological background, the maturity and source of natural gas  from Ake-1 gas pool were discussed by using the results of carbon isotope kine tic modelling. This provided a new thought for evaluating the origin of natural  gas. It's suggested that natural gas of Ake-1 gas pool was the evolution produc t of over-matured source Rocks, with the maturity of 2.0%~3.6% RO, and  belonged to the mixed gas.  

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