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兰州盆地浅部地热水地球化学特征及含氦流体形成机理

唐建洲 王双明 张志诚 李可 李长鹏

煤田地质与勘探2025,Vol.53Issue(6):48-57,10.
煤田地质与勘探2025,Vol.53Issue(6):48-57,10.DOI:10.12363/issn.1001-1986.25.01.0010

兰州盆地浅部地热水地球化学特征及含氦流体形成机理

Geochemical nature of the geothermal water from Lanzhou Basin:Implications for the genesis of shallow helium-bearing fluids

唐建洲 1王双明 2张志诚 3李可 4李长鹏5

作者信息

  • 1. 西安科技大学地质与环境学院,陕西西安 710054||西安石油大学陕西省油气成藏地质学重点实验室,陕西西安 710065||北京大学地球与空间科学学院,北京 100871
  • 2. 西安科技大学地质与环境学院,陕西西安 710054
  • 3. 北京大学地球与空间科学学院,北京 100871
  • 4. 北京大学地球与空间科学学院,北京 100871||重庆大学资源与安全学院,重庆 400044
  • 5. 甘肃省煤田地质局133队,甘肃白银 730913
  • 折叠

摘要

Abstract

[Objective and Methods]Investigations on the geochemical nature of geothermal water are vital to the com-prehension of the origin of helium-rich fluids in shallow basins.To address this issue,this paper reports the results of the chemical analysis,H-O isotopes and 14C ages from geothermal water and soluble gas components from the well BY-1 in Lanzhou Basin,northeastern margin of Qinghai Tibet Plateau.Chemical analysis of geothermal water samples reveals that the chemical type of geothermal water is NaCl.The show δD value of-78‰,high δ18O value(-8.7‰),low 3H value(<0.4TU),and old 14C age(20.50±0.92ka).The geothermal water has undergone evaporation-concentration and water-rock interactions,which originated from ancient atmospheric precipitation.Component analysis from 10 water-dissolved gas samples reveals an average helium concentration of 0.44%.The concentration of He meets the standard for helium-rich gas fields.Compositions of the dissolved gas and the geochemical nature of the groundwater jointly suggest that the associated helium in the geothermal water from this well is a product of the radioactive decay of Th-U elements in the basement rocks of the basin.Comprehensive analysis indicates that the upward migration and accumulation of an-cient helium-bearing water from the basement into shallow geothermal reservoirs along fault zones under the back-ground of tectonic uplift is the key process for the enrichment of associated helium in geothermal water in the Lanzhou Basin.

关键词

氦气/地热水/地球化学特征/新近系杨稍组/兰州盆地/青藏高原东北缘

Key words

helium/geothermal water/geochemistry/Neogene Yangshao Formation/Lanzhou Basin/northeastern mar-gin of Qinghai Tibet Plateau

分类

地质学

引用本文复制引用

唐建洲,王双明,张志诚,李可,李长鹏..兰州盆地浅部地热水地球化学特征及含氦流体形成机理[J].煤田地质与勘探,2025,53(6):48-57,10.

基金项目

陕西省教育厅科学研究计划项目(24JK0547) (24JK0547)

陕西省博士后基金项目(2024BSHSDZZ191) (2024BSHSDZZ191)

陕西省油气成藏地质学重点实验室开放基金项目(PAG-202407) (PAG-202407)

煤田地质与勘探

OA北大核心

1001-1986

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