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Two new geothermal prospects in the Mexican Volcanic Belt: La Escalera and Agua Caliente - Tzitzio geothermal springs, Michoacan, Mexico

机译:墨西哥火山带的两个新地热前景:La Escalera和Agua Caliente-墨西哥米却肯州的Tzitzio地热温泉

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摘要

The La Escalera and Agua-Caliente Tzitzio geothermal areas are newly discovered geothermal prospects in Mexico that may have the potential to be utilized using binary cycle plants. Hot springs (40-50 degrees C) are constrained to the river banks in both areas, but gas discharges occur on the banks as well as in the riverbeds. The thermal water is predominantly bicarbonate type. Reconnaissance work yielded encouraging results, as the Na/K geothermometer indicates temperatures between 139 and 245 degrees C for La Escalera water samples in a partial equilibrium. La Escalera and Tzitzio have strong surface gas discharges, and dry gas samples were collected for delta C-13 isotopic analysis of CH4 and CO2; the results indicate a magmatic origin for the gas discharged.
机译:La Escalera和Agua-Caliente Tzitzio地热区是墨西哥新发现的地热矿床,可能有可能被二元循环电厂利用。温泉(40-50摄氏度)被限制在两个地区的河岸,但是在河岸和河床都发生了气体排放。热水主要为碳酸氢盐类型。侦察工作取得了令人鼓舞的结果,因为Na / K地热仪显示La Escalera水样品处于部分平衡状态时的温度在139到245摄氏度之间。 La Escalera和Tzitzio具有很强的地面气体排放,并且收集了干燥的气体样本用于CH4和CO2的C-13同位素分析。结果表明排出气体的岩浆成因。

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