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<p align="justify"> <br /> <br /> Research area is located in Mt. Manglayang and the surrounding, Sumedang <br /> <br /> Regency, West Java Province, which lies in UTM Zone 48S 801000 – 807000 mE <br /> <br /> and 9235000 - 9241000 mN. This rese...

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Main Author: AULIA RACHMAN (NIM. 12010037), MUHAMAD
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/29070
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:29070
spelling id-itb.:290702018-05-17T14:02:09Z#TITLE_ALTERNATIVE# AULIA RACHMAN (NIM. 12010037), MUHAMAD Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/29070 <p align="justify"> <br /> <br /> Research area is located in Mt. Manglayang and the surrounding, Sumedang <br /> <br /> Regency, West Java Province, which lies in UTM Zone 48S 801000 – 807000 mE <br /> <br /> and 9235000 - 9241000 mN. This research aims to perform detailed geological <br /> <br /> mapping in scale of 1:12.500 as well as identifying the volcanostratigraphy in <br /> <br /> research area. Also to perform resistivity analysis in research area in order to <br /> <br /> determine its correlation with geological mapping result. <br /> <br /> Geomorphological units of research area consists of Manglayang Volcanic <br /> <br /> Cone Unit, Lava Flow Ridge Unit, Lahar Flow Plain Unit, Lahar Flow Ridge Unit, <br /> <br /> and Pyroclastic Flow Ridge Unit. Volcanostratigraphy in research area divided into <br /> <br /> two khuluk there are Khuluk Palasari (Pleistocene epoch) consists of Genteng Lahar <br /> <br /> Breccia (Gb) and Cipanjalu Lahar Breccia (Jb); Khuluk Manglayang (Holocene <br /> <br /> Epoch) consists of Pasir Buluh Pyroclastic Flow Unit (Pa), Banyuresmi Lahar <br /> <br /> Breccia Unit (Bb), Banyuresmi Andesitic Lava Unit 1 (Bl.1), Banyuresmi Andesitic <br /> <br /> Lava 2 (Bl.2), Cilengkrang Andesitic Lava Unit 1 (Cl.1), Cilengkrang Andesitic <br /> <br /> Lava Unit 2 (Cl.2), Cileunyi Wetan Pyroclastic Flow (Wa), Cileunyi Wetan <br /> <br /> Andesitic Lava Unit (Wl). <br /> <br /> Geological model based was made by considring correlation between <br /> <br /> resistivity data analysis and geological field data. Units of geological model consists <br /> <br /> of Soil, Cilengkrang Andesite, Banyuresmi Andesite, Altered Rock, Pyroclastic and <br /> <br /> Lahar. The presence of low resistivity zone indicates altered rock and possibility of <br /> <br /> geothermal potency. <p align="justify"> <br /> text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description <p align="justify"> <br /> <br /> Research area is located in Mt. Manglayang and the surrounding, Sumedang <br /> <br /> Regency, West Java Province, which lies in UTM Zone 48S 801000 – 807000 mE <br /> <br /> and 9235000 - 9241000 mN. This research aims to perform detailed geological <br /> <br /> mapping in scale of 1:12.500 as well as identifying the volcanostratigraphy in <br /> <br /> research area. Also to perform resistivity analysis in research area in order to <br /> <br /> determine its correlation with geological mapping result. <br /> <br /> Geomorphological units of research area consists of Manglayang Volcanic <br /> <br /> Cone Unit, Lava Flow Ridge Unit, Lahar Flow Plain Unit, Lahar Flow Ridge Unit, <br /> <br /> and Pyroclastic Flow Ridge Unit. Volcanostratigraphy in research area divided into <br /> <br /> two khuluk there are Khuluk Palasari (Pleistocene epoch) consists of Genteng Lahar <br /> <br /> Breccia (Gb) and Cipanjalu Lahar Breccia (Jb); Khuluk Manglayang (Holocene <br /> <br /> Epoch) consists of Pasir Buluh Pyroclastic Flow Unit (Pa), Banyuresmi Lahar <br /> <br /> Breccia Unit (Bb), Banyuresmi Andesitic Lava Unit 1 (Bl.1), Banyuresmi Andesitic <br /> <br /> Lava 2 (Bl.2), Cilengkrang Andesitic Lava Unit 1 (Cl.1), Cilengkrang Andesitic <br /> <br /> Lava Unit 2 (Cl.2), Cileunyi Wetan Pyroclastic Flow (Wa), Cileunyi Wetan <br /> <br /> Andesitic Lava Unit (Wl). <br /> <br /> Geological model based was made by considring correlation between <br /> <br /> resistivity data analysis and geological field data. Units of geological model consists <br /> <br /> of Soil, Cilengkrang Andesite, Banyuresmi Andesite, Altered Rock, Pyroclastic and <br /> <br /> Lahar. The presence of low resistivity zone indicates altered rock and possibility of <br /> <br /> geothermal potency. <p align="justify"> <br />
format Final Project
author AULIA RACHMAN (NIM. 12010037), MUHAMAD
spellingShingle AULIA RACHMAN (NIM. 12010037), MUHAMAD
#TITLE_ALTERNATIVE#
author_facet AULIA RACHMAN (NIM. 12010037), MUHAMAD
author_sort AULIA RACHMAN (NIM. 12010037), MUHAMAD
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
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url https://digilib.itb.ac.id/gdl/view/29070
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