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Physiographically, studied area is belong to lowland and hills zone (van Bemmelen, 1949). Geomorphological unit of studied area consist of Anticlinal Ridge and Homoclinal Valley. Rocks in studied area is divided (from the oldest up to the youngest) to claystone with upper delta plain depositinal env...

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Main Author: HIDAYAT (NIM 12005045), FERY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13473
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13473
spelling id-itb.:134732017-09-27T11:46:44Z#TITLE_ALTERNATIVE# HIDAYAT (NIM 12005045), FERY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13473 Physiographically, studied area is belong to lowland and hills zone (van Bemmelen, 1949). Geomorphological unit of studied area consist of Anticlinal Ridge and Homoclinal Valley. Rocks in studied area is divided (from the oldest up to the youngest) to claystone with upper delta plain depositinal environment, tuffaceous sandstone with landword depositinal environment and tuff. Geological structure of this area is anticlinal fold which relatively direction north-south. Coal in studied area consist of six seams with variety thickness from 0.3 to 2.5 m. Based on coal resources calculation with USGS Circular method (Wood, dkk. 1983), has 7,349,141.22 tons measured coal resources and 23,756,797.90 tons indicated coal resources. 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 Physiographically, studied area is belong to lowland and hills zone (van Bemmelen, 1949). Geomorphological unit of studied area consist of Anticlinal Ridge and Homoclinal Valley. Rocks in studied area is divided (from the oldest up to the youngest) to claystone with upper delta plain depositinal environment, tuffaceous sandstone with landword depositinal environment and tuff. Geological structure of this area is anticlinal fold which relatively direction north-south. Coal in studied area consist of six seams with variety thickness from 0.3 to 2.5 m. Based on coal resources calculation with USGS Circular method (Wood, dkk. 1983), has 7,349,141.22 tons measured coal resources and 23,756,797.90 tons indicated coal resources.
format Final Project
author HIDAYAT (NIM 12005045), FERY
spellingShingle HIDAYAT (NIM 12005045), FERY
#TITLE_ALTERNATIVE#
author_facet HIDAYAT (NIM 12005045), FERY
author_sort HIDAYAT (NIM 12005045), FERY
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/13473
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