贵州省高温地热资源形成条件及远景区分析

    Formation conditions and prospective area analysis of high-temperature geothermal resources in Guizhou Province

    • 摘要: 贵州省高温地热资源研究尚处探索阶段,为研究其形成条件与赋存规律,以区域地热勘探资料、钻孔测温数据及重磁解译成果等为基础,系统分析研究区地温梯度、大地热流、储盖组合等关键影响因素。研究表明: 贵州地温梯度整体呈南北高、东西低的特征,平均值为2.4 ℃/100 m,黔西北毕节—金沙、黔西南紫云—望谟及黔东北德江—思南存在显著热异常(3.0~3.5 ℃/100 m); 大地热流值介于30~125 mW/m2,高值区分布于威宁—紫云断裂以西及德江—思南地区,其中威宁矿产勘查区大地热流值实测值达52.8~94.4 mW/m2; 三叠系—寒武系碎屑岩构成区域性低导热盖层(热导率 < 2.5 W/(m·K)),与下伏碳酸盐岩热储形成5个热储单元,黔西南望谟—册亨地区泥盆系—石炭系灰岩储层厚度超过2 000 m,具备优越储热条件。研究圈定黔西北大方—金沙(沉积盆地型)、黔西南望谟—册亨—安龙(高放射性型)及黔西威宁—六盘水(构造活动带型)3个高温地热资源远景区,预测4 500~7 100 m深度温度达150 ℃。研究明确了贵州省高温地热资源的潜力区域与形成条件,可为后续勘查靶区优选与开发利用提供借鉴依据。

       

      Abstract: The research on high-temperature geothermal resources in Guizhou is still in the exploratory stage. To study their formation conditions and occurrence patterns, based on regional geothermal exploration data, borehole temperature measurement data, and gravity and magnetic interpretation results, the authors in this paper have systematically analyzed the key influencing factors such as geothermal gradient, terrestrial heat flow, and reservoir-caprock combinations. The research indicated that the geothermal gradient in Guizhou generally featured higher values in the north and south and lower values in the east and west, with an average of 2.4 ℃/100 m. Significant thermal anomalies (3.0~3.5 ℃/100 m) were observed in Bijie-Jinsha in Northwestern Guizhou, Ziyun-Wangmo in Southwestern Guizhou, and Dejiang-Sinan in Northeastern Guizhou. The terrestrial heat flow values ranged from 30 to 125 mW/m2, with high-value areas being distributed in the western part of Weining-Ziyun Fault and in Dejiang-Sinan region. The measured values in Weining mineral exploration area reached 52.8~94.4 mW/m2. The Triassic to Cambrian clastic rocks constituted a regional low-thermal-conductivity caprock (thermal conductivity < 2.5 W/(m·K)), forming five sets of reservoir-caprock combinations with the underlying carbonate rock reservoirs. The Devonian-Carboniferous limestone reservoirs in Wangmo-Ceheng area in southwestern Guizhou were over 2000 m thick, providing excellent thermal storage conditions. This study comprehensively delineated three prospective areas of high-temperature geothermal resources in Guizhou Province, including Dafang-Jinsha area in Northwestern Guizhou (sedimentary basin type), Wangmo-Ceheng-Anlong area in Southwestern Guizhou (high radioactive type), and Weining-Liupanshui area in Western Guizhou (tectonic active zone type). The study predicted that the temperature could reach 150 ℃ at the depth of 7 100~7 900 m. The study clarifies the potential areas and formation conditions of high-temperature geothermal resources in Guizhou Province, providing some references for subsequent exploration target area optimization and development and utilization.

       

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