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The study area is divide into three geomorphology unit which is, Volcanic hill unit, Folding hill unit, and aluvial terrain. Ther river in this area is rectangular type. Stratigraphically the research area is divided into five lithostratigraphy unit, those lithostratigraphy unit are (from the oldest...

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Main Author: ADI (NIM 12004023), KURNIA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13607
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13607
spelling id-itb.:136072017-09-27T11:46:45Z#TITLE_ALTERNATIVE# ADI (NIM 12004023), KURNIA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13607 The study area is divide into three geomorphology unit which is, Volcanic hill unit, Folding hill unit, and aluvial terrain. Ther river in this area is rectangular type. Stratigraphically the research area is divided into five lithostratigraphy unit, those lithostratigraphy unit are (from the oldest to the youngest): Limestone unit (Rajamandala Formation) Sandstone – Claystone unit (Citarum Formation), Volcanic breccia (Saguling Formation), Tuff unit. The geology structure which develop in this area are thrust fault, strike slip, and fold. The thrust fault and the fold axis has an relatively east – west orientation. The strike slip fault has an relatively NW – SE trend. Those geological structure was intrepted as a fold – thrust related system. 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 The study area is divide into three geomorphology unit which is, Volcanic hill unit, Folding hill unit, and aluvial terrain. Ther river in this area is rectangular type. Stratigraphically the research area is divided into five lithostratigraphy unit, those lithostratigraphy unit are (from the oldest to the youngest): Limestone unit (Rajamandala Formation) Sandstone – Claystone unit (Citarum Formation), Volcanic breccia (Saguling Formation), Tuff unit. The geology structure which develop in this area are thrust fault, strike slip, and fold. The thrust fault and the fold axis has an relatively east – west orientation. The strike slip fault has an relatively NW – SE trend. Those geological structure was intrepted as a fold – thrust related system.
format Final Project
author ADI (NIM 12004023), KURNIA
spellingShingle ADI (NIM 12004023), KURNIA
#TITLE_ALTERNATIVE#
author_facet ADI (NIM 12004023), KURNIA
author_sort ADI (NIM 12004023), KURNIA
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/13607
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