IDENTIFICATION OF FAULT CONTINUITY AND HOT WATER RESERVOIR USE SCHLUMBERGER CONFIGURATION RESISTIVITY METHOD IN CANGAR

Dhony Widyasandy, A. K. Nugraha, Husni Cahyadi Kurniawan, Ahmad Luthfin
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Abstract

Research that uses the Schlumberger configuration resistivity method had been conducted in Cangar. The purpose of this study is to identify cracks/faults and potential hot springs use resistivity well analysis and correlate it with rock lithology in Cangar, East Java. Data acquisition is carried out using 3 tracks with 10 sounding points. The space between points is 50 meters. The rock resistivity values obtained were 9945 Ωm, 7360 Ωm, and 5573 Ωm which were thought to be breccia layers and functioned as hot springs. This estimation is strengthened by the existence of a layer of breccia-andesite because this layer is very good as a water reservoir. In addition, based on the lateral cross-section on lane 1, there was a decrease in boulder-sized breccia-andesite layers; this decrease was the production of faults.
利用斯伦贝谢组态电阻率法在坎加进行断层连续性和热水储层的识别
使用斯伦贝谢组态电阻率法在canar进行了研究。本研究的目的是利用电阻率井分析识别裂缝/断层和潜在的温泉,并将其与东爪哇canar的岩石岩性相关联。数据采集采用3道10测深点。点与点之间的距离为50米。得到的岩石电阻率值分别为9945 Ωm、7360 Ωm和5573 Ωm,认为为角砾岩层,具有温泉功能。角砾岩安山岩层的存在加强了这一估计,因为这一层具有很好的储水能力。此外,从1巷的横向剖面来看,砾石级角砾岩安山岩层数减少;这种减少是断层的产物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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