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塔里木盆地阿克1气藏天然气的地球化学特征和成因

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

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【作者】 李贤庆肖贤明肖中尧胡国艺米敬奎唐永春

【Author】 LI Xian-qing~(1,2), XIAO Xian-ming~2, XIAO Zhong-yao~3, HU Guo-yi~4, MI Jing-kui~2, TANG Yong-chun~5versity of Mining and Technology,gzhou Institute ofGeochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 3.The Research Institute ofExploration and Development, Tarim Oil Field Company, CNPC, Kuerle 841000, China;4.Institute ofNatural Gas Geology, Langfang Branch, Research Institute of Petroleum Exploration and Development, CNPC,Langfang 065007, China;5.The Research Center of Petroleum Energy and Enviroment, California Institute ofTechnology, California 91789, USA)

【机构】 中国矿业大学煤炭资源教育部重点实验室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中国石油塔里木油田分公司勘探开发研究院中国石油勘探开发研究院廊坊分院天然气地质研究所美国加利福尼亚州理工学院石油能源与环境研究中心 北京 1 0 0 0 83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 51 0 640新疆库尔勒 841 0 0 0河北廊坊 0 650 0 7广东广州 51 0 640美国加利福尼亚 91 789

【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。

【Abstract】 Ake-1 is a commercial gas pool that has made great breakthrough for oil & gas exploration 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 belongs to the typical dry gas. It has predominance methane (80%~91%), low content 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 ethane (-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 kinetic 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 product of over-matured source Rocks, with the maturity of 2.0%~3.6% RO, and belonged to the mixed gas.

【基金】 国家"十五"重点科技攻关项目(编号:2001BA605A02-03-01);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.
  • 【文献出处】 天然气地球科学 ,Natural Gas Geoscience , 编辑部邮箱 ,2005年01期
  • 【分类号】TE122.113
  • 【被引频次】11
  • 【下载频次】375
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