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Hydrogeochemical characteristics at Dona Juana Complex (SW Colombia): A new area for geothermal exploration in the Northern Andes region

机译:Dona Juana Complex(哥伦比亚西南部)的水文地球化学特征:北安第斯山脉地区的地热勘探新区

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摘要

The Doha Juana Volcanic Complex (DJVC) is an active volcanic zone located in southern Colombia, an area lacking geothermal exploration data. Using the results of hydrogeochemical analyses of hot springs, thermal waters were divided into two groups: Doha Juana System (DJS) and Las Animas System (AS). The DJS thermal waters are sulphate-bicarbonate and the AS dilute-chloride waters with relatively high concentrations of alkalis. The stable isotope and some element ratios suggested a mixing process between geothermal fluids and meteoric waters where AS is related to the upflow with a reservoir temperature around 180 degrees C estimated through solute geothermometers and mineral equilibrium geothermometry, showing a high temperature system in which the fault systems apparently play an important role in the flow of the geothermal fluids.
机译:多哈胡安娜火山综合体(DJVC)是位于哥伦比亚南部的活跃火山带,该地区缺少地热勘探数据。利用温泉的水文地球化学分析结果,将温泉水分为两类:多哈胡安娜系统(DJS)和拉斯阿尼玛斯系统(AS)。 DJS热水是硫酸氢盐和碳酸氢盐,而AS稀氯水具有较高的碱浓度。稳定的同位素和某些元素比率表明地热流体与流域水之间存在混合过程,其中AS与向上流动有关,通过溶质地热仪和矿物平衡地热仪估计储层温度约为180摄氏度,这表明存在断层的高温系统系统显然在地热流体的流动中起着重要的作用。

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