#TITLE_ALTERNATIVE#
<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...
Saved in:
| Main Author: | |
|---|---|
| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/29070 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | <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 />
|
|---|