ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    柴达木盆地水溶氦气资源的发现及富集机理

    晁海德, 陈建洲, 王国仓, 赵维孝, 蔡廷俊, 李吉庆, 李青, 谢菁

    晁海德, 陈建洲, 王国仓, 等. 柴达木盆地水溶氦气资源的发现及富集机理[J]. 西北地质, 2022, 55(4): 61-73. DOI: 10.19751/j.cnki.61-1149/p.2022.04.005
    引用本文: 晁海德, 陈建洲, 王国仓, 等. 柴达木盆地水溶氦气资源的发现及富集机理[J]. 西北地质, 2022, 55(4): 61-73. DOI: 10.19751/j.cnki.61-1149/p.2022.04.005
    CHAO Haide, CHEN Jianzhou, WANG Guocang, et al. Discovery and Enrichment Mechanism of Water Soluble Helium Resources in Qaidam Basin[J]. Northwestern Geology, 2022, 55(4): 61-73. DOI: 10.19751/j.cnki.61-1149/p.2022.04.005
    Citation: CHAO Haide, CHEN Jianzhou, WANG Guocang, et al. Discovery and Enrichment Mechanism of Water Soluble Helium Resources in Qaidam Basin[J]. Northwestern Geology, 2022, 55(4): 61-73. DOI: 10.19751/j.cnki.61-1149/p.2022.04.005

    柴达木盆地水溶氦气资源的发现及富集机理

    基金项目: 

    青海省地质矿产勘查开发局地质勘查项目“青海省清洁能源靶区优选”(青地矿科〔2020〕61、青地矿科〔2021〕61、青地矿科〔2022〕32)资助。

    详细信息
      作者简介:

      晁海德(1987-),男,工程师,从事能源矿产勘查、研究工作。E-mail:394262585@qq.com。

    • 中图分类号: P618.13

    Discovery and Enrichment Mechanism of Water Soluble Helium Resources in Qaidam Basin

    • 摘要: 通过采集、测试柴达木盆地卤水井、温泉水样品,以及氦源岩及其生氦强度研究,梳理水溶性氦气分布特征,总结成因,探究富集机理,以期了解柴达木盆地水溶性氦气资源现状,并拓展氦气藏勘探、研究的新思路。结果表明:柴达木盆地氦源岩是多元的、开放的,除花岗岩外,侏罗纪、石炭纪泥页岩是潜在的生氦母岩,且侏罗纪泥页岩生氦强度最大,志留纪二长花岗岩次之,石炭纪泥页岩最低;以油砂山组、狮子沟组为主要聚集层的水溶性氦气分布于柴中断裂以北区域,且存在北、中、南3条控氦断裂带;柴达木盆地水溶性氦气基本为壳源型氦气,幔源氦仅占0.005%~0.42%;水溶性氦气成藏的关键在于“生、运、储”,其中泥页岩、中酸性岩体是氦气潜在生成母源,地下水、断裂提供运移载体及通道,油砂山组、狮子沟组提供储集空间。
      Abstract: By collecting and testing brine wells and hot spring water samples in the Qaidam basin, the source rock of water-soluble helium and its helium generation intensity have been explored. The results show that the helium source rocks in the Qaidam basin are diverse and open. In addition to granite, Jurassic and Carboniferous shale are indispensable helium-generating parent rocks, and Jurassic shale is helium-generating. The strength is the highest, followed by the Silurian monzogranite, and the Carboniferous shale is the lowest; the water-soluble helium enrichment areas with the Youshashan Formation and Shizigou Formation as the main enrichment layers are distributed in the area north of the Chaizhong fault, and There are three helium-controlling fault zones in the north, middle, and south; the water-soluble helium in the Qaidam basin is basically crust-derived helium, and the mantle-derived helium only accounts for 0.005%~0.42%; “transportation and storage” is the key factors for water-soluble helium resources, in which shale and medium-acid rock mass are the parent sources of helium gas generation, groundwater and faults provide migration carriers and channels, and the Youshashan Formation and Shizigou Formation provide storage space.
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    出版历程
    • 收稿日期:  2022-06-13
    • 修回日期:  2022-08-21
    • 网络出版日期:  2023-01-09

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