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This research area is divided into two geomorphological units: Complex Mountain Unit and Coastal Plain Unit. Stratigraphy in research area is divided into four units: Middle Eocene Conglomeratic Sandstone Unit, Late Oligocene Sandstone Unit, Early Pliocene Conglomerate Unit, and Recent Aluvial-Coast...

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Main Author: MUSTIKA SUCIATI (NIM 12005055), RISCA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13788
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13788
spelling id-itb.:137882017-09-27T11:46:39Z#TITLE_ALTERNATIVE# MUSTIKA SUCIATI (NIM 12005055), RISCA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13788 This research area is divided into two geomorphological units: Complex Mountain Unit and Coastal Plain Unit. Stratigraphy in research area is divided into four units: Middle Eocene Conglomeratic Sandstone Unit, Late Oligocene Sandstone Unit, Early Pliocene Conglomerate Unit, and Recent Aluvial-Coastal Deposit. Geological structures formed in the research area are reverse faults, strike slip faults, and folds. Research area is a part of fold-thrust belt which has formed by compressive tectonic. Reverse fault is the main structure in the research area, with strike slip faults and folds as accompaniment structures. Strike slip faults were formed by each block ability differences to accommodate compressive force. 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 This research area is divided into two geomorphological units: Complex Mountain Unit and Coastal Plain Unit. Stratigraphy in research area is divided into four units: Middle Eocene Conglomeratic Sandstone Unit, Late Oligocene Sandstone Unit, Early Pliocene Conglomerate Unit, and Recent Aluvial-Coastal Deposit. Geological structures formed in the research area are reverse faults, strike slip faults, and folds. Research area is a part of fold-thrust belt which has formed by compressive tectonic. Reverse fault is the main structure in the research area, with strike slip faults and folds as accompaniment structures. Strike slip faults were formed by each block ability differences to accommodate compressive force.
format Final Project
author MUSTIKA SUCIATI (NIM 12005055), RISCA
spellingShingle MUSTIKA SUCIATI (NIM 12005055), RISCA
#TITLE_ALTERNATIVE#
author_facet MUSTIKA SUCIATI (NIM 12005055), RISCA
author_sort MUSTIKA SUCIATI (NIM 12005055), RISCA
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/13788
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