矿物岩石地球化学通报2024,Vol.43Issue(1) :167-177.DOI:10.3724/j.issn:1007-2802.20240010

柴北缘大柴旦地区地下热水成因:来自水化学及氢、氧、锶同位素的约束

Gensis of geothermal water in the Da Qaidam area,northern margin of the Qaidam Basin:Constraints from hydrochemistry and isotopes of hydrogen-oxygen-strontium

王兵 秦西伟 任二峰 蒋子文 冯宁 李国荣 杨莎 李玮
矿物岩石地球化学通报2024,Vol.43Issue(1) :167-177.DOI:10.3724/j.issn:1007-2802.20240010

柴北缘大柴旦地区地下热水成因:来自水化学及氢、氧、锶同位素的约束

Gensis of geothermal water in the Da Qaidam area,northern margin of the Qaidam Basin:Constraints from hydrochemistry and isotopes of hydrogen-oxygen-strontium

王兵 1秦西伟 2任二峰 2蒋子文 2冯宁 1李国荣 2杨莎 2李玮2
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作者信息

  • 1. 青海大学 地质工程系,西宁 810016
  • 2. 青海大学 地质工程系,西宁 810016;青藏高原北缘新生代资源环境重点实验室,西宁 810016
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摘要

为探究柴达木盆地北缘的大柴旦地热田的水化学特征及成因模式,本文对研究区14组地下热水进行了水化学组分和同位素(δD,δ18O,87Sr/86Sr,3H)分析.结果表明,大柴旦地下热水出露温度为52~74℃,溶解性总固体浓度(TDS)为959.8~1451.3 mg/L.地下热水的水化学类型为Cl-Na型,区内地下热水的水化学成分主要来源于蒸发岩和硅酸盐矿物的溶解;氢、氧稳定同位素特征表明,大气降水及冰雪融水是地下热水主要补给来源,且部分温泉有岩浆水的补给,估算的补给高程为3591~4374 m.3H测年结果表明,区内地下热水主要由1952年之前的古水补给、蒸发作用和水-岩反应增强导致.XSWQ-06和XSWQ-07样品有明显的氧漂移.基于SiO2地热温标、多矿物平衡法和硅焓模型估算出的地下热水的热储温度为171~227℃,循环深度为4.7~6.9 km.该地区地热资源具有较大的开发利用潜力.

Abstract

In order to explore the hydrochemical characteristics and genetic model of the geothermal field in Da Qaidam,the northern margin of the Qaidam basin,14 groups of groundwater sample of this area were analyzed for hydrochemical components and isotopes(δD,δ18O,87Sr/86Sr,3H)in this study.The results show that the outlet temperature of underground hot water in Da Qaidam is 52~74℃,and the total dissolved solids(TDS)content is 959.8~1451.3 mg/L.The hydrochemical types of the groundwater are all the Cl-Na type,and according to the ion correlation and 87Sr/86Sr value,the main solutes of groundwater in the area originate from the dissolution of evaporites and silicate minerals.Stable isotopes of hydrogen and oxygen show that atmospheric precipitation is the main source of groundwater recharge and part of the groundwater is recharged by magma water,and the estimated recharge elevation is 3591~4374 m.XSWQ-06 and XSWQ-07 have significant oxygen drift,mainly due to evaporation and enhanced water-rock reaction.Based on the SiO2 geothermal temperature scale,the multi-mineral equilibrium method and the silicon enthalpy model,the thermal storage temperature of underground hot water in the area is estimated to be 171~227℃,and the circulation depth is estimated to be 4.7~6.9 km.The geothermal resources in this area have great potential for development and utilization.

关键词

水文地球化学/地下热水/热储温度/成因分析/大柴旦

Key words

hydrogeochemistry/hot spring/reservoir temperatures/genesis analysis/Da Qaidam

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基金项目

青海省科技计划(2021-ZJ-937Q)

出版年

2024
矿物岩石地球化学通报
中国矿物岩石地球化学学会 中国科学院地球化学研究所

矿物岩石地球化学通报

CSTPCDCSCD北大核心
影响因子:0.912
ISSN:1007-2802
参考文献量35
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