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Analysis Geothermal Prospect of Mt. Endut Using Geochemistry Methods

机译:使用地球化学方法分析MT的地热前景。

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Mt. Endut geothermal area is located in Lebak district, Banten province, about 40 km to the south of the town of Rangkasbitung. There are four manifestations of hot springs i.e: Handeuleum hot springs, Cikawah 1, Cikawah 2, and Gajrug. Based on geochemical analysis using Na-K-Mg triangular diagrams, Cl-Li-B, and C1-SO4-HCO3, it is known that Cikawah 1 hot springs is chloride type and the other springs are bicarbonate type. Reservoir temperature range is from 162°C to 180°C are predicted by SiO2 and NaK geothermometers. In general all hot springs are out flows, but there is an hypothesis that Cikawah 1 is the up flow. Because it is in partial equilibrium and chloride type. Mount Endut has a hydrothermal system with a fluid reservoir in the form of hot water or water dominated system. The geothermal prospect area of Mount Endut is located around the Cikawah manifestation to the western part of the Endut mountain. Further research is required by conducting geophysical surveys around the Mount Endut.
机译:Mt.DeDut地热区位于Banten Province lebak区,距离Rangkasbitung镇南部约40公里。温泉有四个表现形式:Handeuleum Hot Springs,Cikawah 1,Cikawah 2和Gajrug。基于使用Na-K-Mg三角形图的地球化学分析,Cl-Li-B和C1-SO4-HCO3,已知Cikawah 1热弹簧是氯化物型,另一个弹簧是碳酸氢盐型。储层温度范围为162°C至180℃,通过SiO2和Nak地热测量预测。一般而言,所有温泉都是流动的,但有一个假设是Cikawah 1是上升的流动。因为它处于部分平衡和氯化物类型。安装终止具有热水或水主导系统形式的流体储存器的水热系统。登山山上的地热前景区域位于雪川表现形式,到终止山的西部。通过在登山终止周围进行地球物理调查来进行进一步的研究。

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