徐玉华, 唐振芳, 宋峰, 王志强, 王先彬, 陈践发. 宁镇地区稀有气体中He同位素分析的初步结果[J]. 华北地震科学, 1993, 11(2): 89-94.
引用本文: 徐玉华, 唐振芳, 宋峰, 王志强, 王先彬, 陈践发. 宁镇地区稀有气体中He同位素分析的初步结果[J]. 华北地震科学, 1993, 11(2): 89-94.
Xu Yuhua, Tang Zhenfang, Song Feng, Wang Zhiqiang, Wang Xianbin, Chen Jianfa. PRELIMINARY RESULT OF ANALYSIS OF HE ISOLOPE IN RARE GAS IN NINGZHEN AREA[J]. North China Earthquake Sciences, 1993, 11(2): 89-94.
Citation: Xu Yuhua, Tang Zhenfang, Song Feng, Wang Zhiqiang, Wang Xianbin, Chen Jianfa. PRELIMINARY RESULT OF ANALYSIS OF HE ISOLOPE IN RARE GAS IN NINGZHEN AREA[J]. North China Earthquake Sciences, 1993, 11(2): 89-94.

宁镇地区稀有气体中He同位素分析的初步结果

PRELIMINARY RESULT OF ANALYSIS OF HE ISOLOPE IN RARE GAS IN NINGZHEN AREA

  • 摘要: 本文主要报告南京——镇江地区5个采样点3He/4He比值重复测量结果,它们在(6.18±0.17)×10-6至(3.12±0.08)×10-7之间变化。最高值来自42C左右热泉(汤泉)的气泡气、最低值来自人工钻孔——句容自流水水溶气。
    5个点的3He/4He比值(Rs)可分成两种类型、一类Rs值明显高于大气中3He/4He值(Ratm),分别是4.4Ratm和4.1Ratm,这是本项研究中首次测到的。另一类则低于Ratm。
    以上两种类型气体Rs的差异,反映了气体的来源和成因上的差异,也反映了采样点地质背景特征的不同,本区温泉气体中Rs的高值可能与新生代以来的岩浆活动有关,是富3He的原始的幔源He仍在继续从地球深处向外排放的证据。

     

    Abstract: The paper reported the repeatedly measured result of 3He/4 ratio for the gas samples collected from 5 springs and artesian wells in Nanjing—Zhenjiang region.The values of the ratios are variable, ranging from (6.18±0.17)×10-6to (3.12±0.08)×10-7。The highest value appears in bubbling gases of the hot spring (42UC±) at Tangquan, and the lowest in the artesian well at Jurong.
    3He/4 ratios (Rs) for gas samples collected from 5 sites can be grouped into two types.In one type, the He/4He ratios of bubbling gases of two hot springs are obviously higher than the atmospheric ratio (Ratm), being 4.4 Ratm and 4.1 Ratm respectively.The high 3He/4 ratios were first observed in this study.In another type, they are lower than Ratm.
    The above difference of two type gases Rs reflects the difference in source and origin of gas samples and the difference in geological setting property of the sites where samples were collected.The high 3He/4 value of hot spring gases in this area may be related to magmatic activity since Cenozoic.It is an evidence that the primordial 3He of He—rich is still emanating from the deep interior of the earth.

     

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