Cimandiri fault is an active fault indicated by the appearance of hot springs that prove the presence of geothermal activity. The hot springs have different temperature due to physical characteristics in each location. The purpose of this research is to find geothermal prospective region based on physical characteristics at Cimandiri fault, West Java. This research uses integrated survey methods between geography, geology, and geochemical aspects with remote sensing technology. Remote sensing used in analyzing Land Surface Temperature in research areas. The Geochemical survey is done by collecting hot spring samples to get consentration of the Na and K elements. The data latter are used in counting reservoir temperature using Geothermometry method. The results concluded that there are three geothermal prospective regions in Cimandiri Fault classified in low and moderate levels. The low geothermal prospective region is represented in Cibubuay region with reservoir temperature of ...

中文翻译：

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西爪哇西曼迪里断裂带基于物理特征的地热勘探区，基于遥感

Cimandiri断层是活跃的断层，其特征是温泉的出现证明了地热活动的存在。由于每个位置的物理特性，温泉的温度不同。这项研究的目的是根据西爪哇Cimandiri断层的物理特征找到地热前兆区域。这项研究使用遥感技术在地理，地质和地球化学方面之间使用集成的调查方法。遥感技术用于研究区域的地表温度分析。地球化学调查是通过收集温泉样品以获取Na和K元素的同意来进行的。后面的数据用于通过地热法对储层温度进行计数。结果表明，在Cimandiri断层中有3个地热潜在区域，分为中低水平。地热布依地区为地热低发区，储层温度为...