CONCEPTUAL MODEL OF THE “UBL” REGION GEOTHERMAL SYSTEM OF LAMPUNG PROVINCE USING DRILL LOG DATA AND SURFACE MANIFESTATION GEOCHEMICALS

Muhammad Aisy Omar, F. Hendrasto, Graniko Reza Utama
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Abstract

The UBL area is included in the Tanggamus Regency, Lampung province, with the potential for geothermal resources. The study of geothermal in the UBL area continues to increase along with the existence of geothermal operating areas that have been proven to produce geothermal energy that is capable of being used as a Geothermal Power Plant (PLTP). Therefore, this research was conducted to look in more detail through surface data and subsurface data so that it can provide an overview of the geothermal model in this "ULB" area. Surface fluid manifestations show 3 types of springs, namely chloride water, sulfate water, and bicarbonate water. The main reservoir of the study area is diorite-basalt intermediate rock. It is estimated that the reservoir temperature ranges from 184.31O – 200.56O C. The geothermal system model shows the upflow zone in the north of the study area covering the Aek Besuk area (AB2) and the outflow zone in the southern part of the Batu Rejo area (BR2).
基于测井资料和地表地表地球化学特征的楠榜省“ubl”地区地热系统概念模型
UBL地区包括在楠榜省的Tanggamus Regency,具有地热资源的潜力。随着地热作业区域的存在,对UBL地区地热的研究不断增加,这些地热作业区域已被证明可以产生能够用作地热发电厂(PLTP)的地热能。因此,本研究通过地表数据和地下数据进行更详细的研究,以便对该“ULB”地区的地热模式进行概述。地表流体表现为氯化物水、硫酸盐水和碳酸氢盐水3种类型的泉水。研究区主要储层为闪长岩-玄武岩中间岩。储层温度范围为184.31 ~ 200.56℃。地热系统模型显示研究区北部为上流区,覆盖Aek Besuk区(AB2),南部为流出区,覆盖Batu Rejo区(BR2)。
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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