| Origin of Natural Gas in Kekeya Field, Tarim Basin, China |
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| 引用本文： | HouDujie XiaoZhongyao TangYoujun ZhuJunzhang LiXianqing. Origin of Natural Gas in Kekeya Field, Tarim Basin, China[J]. 中国地质大学学报(英文版), 2004, 15(1): 91-98 |
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| 作者姓名： | HouDujie XiaoZhongyao TangYoujun ZhuJunzhang LiXianqing |
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| 作者单位： | [1]EnergyResourceDepartment,ChinaUniversityofGeosciences,Beijing100083,China [2]TarimPetroleumExplorationBureau,Kuerle841000,China [3]GeochemistryResearchCenter,YangtzeUniversity,Jingzhou434023,China |
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| 基金项目： | 国家重点基础研究发展计划(973计划)，Tarim Petroleum Research Foundation |
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| 摘 要： | This paper is mainly concentrated on the geochemical characteristics and origin of gas of Kekeya field in the Tarim basin, NW China. This study shows that Permian mudstone is the main source rock of oil and gas. Based on the carbon isotopes of C1--C4, the carbon isotope of gas in Kekeya field is a little heavier than that in the typical marine-derived gas. The relationship between carbon isotopes of methane and ethane is coincident with Faber equation of gas derived from organic matter Ⅰ/Ⅱ. The majority of gas maturity is estimated, based on the formula, at 1.8%-2.2% besides K2 and K18 wells. In addition, the gas derived from 0.9%-1.2% Ro source rocks may also bemixture. ^40Ar/^36Ar and ^3He/^4He ratios from the gas samples also support the mixing process. Moreover, the gas in this region is mainly generated from more mature source rocks although the low mature gas exists.
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| 关 键 词： | 天然气 地球化学 塔里木盆地 二叠纪 |
Origin of Natural Gas in Kekeya Field, Tarim Basin, China |
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| Hou Dujie,Xiao Zhongyao,Tang Youjun,Zhu Junzhang,Li Xianqing. Origin of Natural Gas in Kekeya Field, Tarim Basin, China[J]. Journal of China University of Geosciences, 2004, 15(1): 91-98 |
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| Authors: | Hou Dujie Xiao Zhongyao Tang Youjun Zhu Junzhang Li Xianqing |
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| Abstract: | This paper is mainly concentrated on the geochemical characteristics and origin of gas of Kekeya field in the Tarim basin, NW China. This study shows that Permian mudstone is the main source rock of oil and gas. Based on the carbon isotopes of C1-C4, the carbon isotope of gas in Kekeya field is a little heavier than that in the typical marine-derived gas. The relationship between carbon isotopes of methane and ethane is coincident with Faber equation of gas derived from organic matter Ⅰ/Ⅱ. The majority of gas maturity is estimated, based on the formula, at 1.8 %-2.2 % besides K2 and K18 wells. In addition, the gas derived from 0.9 %-1.2 % Ro source rocks may also be mixture. 40Ar/36Ar and 3He/4He ratios from the gas samples also support the mixing process. Moreover, the gas in this region is mainly generated from more mature source rocks although the low mature gas exists. |
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| Keywords: | natural gas origin Kekeya source rock |
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