地质地热区Pangi Kabupaten Bone Bolango省Gorontalo

Dewi Darmayanti Tolodo, Fauzul Chaidir A. Usman, Intan Noviantari Manyoe, F. Gaib, Fitri Handayani Putje, Yusran Ibrahim
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引用次数: 3

摘要

地热与地表以下仍有热能的火山岩有关。印度尼西亚是一个地热能储量约为40%的国家。有256个潜在的地热区,只有7个位置被利用。Gorontalo有几种地热表现,如Lombongo、Pangi、Libungo和Hungayono。本研究的目的是研究戈伦塔洛省Bone Bolango县东Suwawa区Pangi的地热表现地质。研究方法分为实地观察、实验室分析和工作室分析。研究结果表明,研究区的地貌可分为3个单元,即冲积平原、火山丘和构造利用景观。冲积沉积单元、火山角砾岩单元、塔夫-拉皮利单元、安山岩单元、花岗闪长岩单元和斑岩-闪长岩。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geologi Daerah Geothermal Pangi Kabupaten Bone Bolango Provinsi Gorontalo
Geothermal is associated with volcanic that still has heat energy below the surface. Indonesia is a country with geothermal energy reserves of around 40%. There are 256 potential geothermal areas and only 7 locations have been utilized. Gorontalo has several geothermal manifestations, such as Lombongo, Pangi, Libungo, and Hungayono. The purpose of this study was to study the geology of the geothermal manifestations of Pangi, East Suwawa District, Bone Bolango Regency, Gorontalo Province. The research method is divided into field observations, laboratory analysis, and studio analysis. The results of this research show that the geomorphology in the study area is divided into 3 units, namely the Fluvial Plain, the Volcanic Hills, and the Structural Use Landscape. Alluvial Deposition Unit, Volcanic Breccia Unit, Tuff Lapili Unit, Andesite Unit, Granodiorite Unit, and Porphyry Diorite Unit.
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