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天然气中氦同位素分布及构造环境
引用本文:徐永昌.天然气中氦同位素分布及构造环境[J].地学前缘,1997(Z2).
作者姓名:徐永昌
作者单位:中国科学院兰州地质研究所气体地球化学国家重点实验室
摘    要:通过采集天然气样334个,测量了它们的氦同位素组成。3He/4He值分布在056×10-8~721×10-6范围。3He/4He值分布与天然气储层时代无明显的相关性,而在空间展布上有较明显的规律。东部含油气区3He/4He值主要分布于10-7~10-6范围,西部含油气区在10-7~10-8的范围,中部地区分布在056×10-9~056×10-8范围,3He/4He值的分布与我国构造环境大的格局有很好的相关性。3He/4He的高值区构造环境活动性强,低值区具有最稳定的大地构造属性,西部地区3He/4He值介于东部和中部,具有次稳定的构造环境。

关 键 词:天然气  氦同位素  构造环境

HELIUM ISOTOPE DISTRIBUTION OF NATURAL GASSES AND ITS STRUCTURAL SETTING
Xu Yongchang.HELIUM ISOTOPE DISTRIBUTION OF NATURAL GASSES AND ITS STRUCTURAL SETTING[J].Earth Science Frontiers,1997(Z2).
Authors:Xu Yongchang
Abstract:Based on the research of the helium isotope composition within 334 natural gas samples, it is found that the 3He/ 4He ratio is 0.56×10 -8 ~7.21×10 -6 . Though there is no evident relativity between the distribution of 3He/ 4He ratio and the age of natural gas reservoir, but indeed the ratio distributes regularly in space. In general, the 3He/ 4He ratio is 10 -7 ~10 -6 in the oil gas bearing area in East China, 10 -7 ~10 -8 in West China and 0.56×10 -9 ~0.56×10 -8 in midland. The distribution of 3He/ 4He ratio is distinctly related to the structural setting. The area of higher 3He/ 4He ratio is the most active structural setting, the area of lower 3He/ 4He ratio is the most stable and the midland is the sub stable one, where the 3He/ 4He ratio is between the East and West of China.
Keywords:natural gas  helium isotope  structural setting
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