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Depending on morfological shape and process in research area, this area devide into four geomorfological units, which is Anticline Mountain Unit, Fault Scarp Unit, Fold Limb Mountain Unit, and Flood Plain Unit. Stratigraphy units in research area consist of Massive Sandstone Unit, Bedding Sandstone...

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Main Author: RULLY AMARULLAH (NIM 12006012), ZULFIKAR
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13925
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13925
spelling id-itb.:139252017-09-27T11:46:39Z#TITLE_ALTERNATIVE# RULLY AMARULLAH (NIM 12006012), ZULFIKAR Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13925 Depending on morfological shape and process in research area, this area devide into four geomorfological units, which is Anticline Mountain Unit, Fault Scarp Unit, Fold Limb Mountain Unit, and Flood Plain Unit. Stratigraphy units in research area consist of Massive Sandstone Unit, Bedding Sandstone Unit, Claystone Unit, and Alluvium Unit. That stratigraphy units equal with three formation, Batupasir Haloq in Late Eocene, Batu Ayau Formation in Late Eocene, and Ujoh Bilang Formation in Early Oligosen (Abidin, et al., 1993). Structures in research area consist of fault and fold, Leng Normal Fault with N-S direction, Merah Strike Slip Fault with NW-SE direction, and Leng Anticline with NE-SW fold axis. 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 Depending on morfological shape and process in research area, this area devide into four geomorfological units, which is Anticline Mountain Unit, Fault Scarp Unit, Fold Limb Mountain Unit, and Flood Plain Unit. Stratigraphy units in research area consist of Massive Sandstone Unit, Bedding Sandstone Unit, Claystone Unit, and Alluvium Unit. That stratigraphy units equal with three formation, Batupasir Haloq in Late Eocene, Batu Ayau Formation in Late Eocene, and Ujoh Bilang Formation in Early Oligosen (Abidin, et al., 1993). Structures in research area consist of fault and fold, Leng Normal Fault with N-S direction, Merah Strike Slip Fault with NW-SE direction, and Leng Anticline with NE-SW fold axis.
format Final Project
author RULLY AMARULLAH (NIM 12006012), ZULFIKAR
spellingShingle RULLY AMARULLAH (NIM 12006012), ZULFIKAR
#TITLE_ALTERNATIVE#
author_facet RULLY AMARULLAH (NIM 12006012), ZULFIKAR
author_sort RULLY AMARULLAH (NIM 12006012), ZULFIKAR
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/13925
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