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Morphology of this area is divided into four geomorphology units: Fold Hills Unit, Homoclinal Plain Unit, Intrusive Hills Unit is characterized by steep slopes and consists of granite, Alluvial Plain Unit is showed by plain morphology that lies alongside Buluhrotan River flow. The Stratigraphy of th...

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Main Author: FERNANDO BUTARBUTAR (NIM 12007007), ELREY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13426
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13426
spelling id-itb.:134262017-09-27T11:46:45Z#TITLE_ALTERNATIVE# FERNANDO BUTARBUTAR (NIM 12007007), ELREY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13426 Morphology of this area is divided into four geomorphology units: Fold Hills Unit, Homoclinal Plain Unit, Intrusive Hills Unit is characterized by steep slopes and consists of granite, Alluvial Plain Unit is showed by plain morphology that lies alongside Buluhrotan River flow. The Stratigraphy of this area is divided into five illegitimate units of lithostratigraphy. The following are sorted from the oldest to the youngest, those are: Pre- Tertiary Granite Unit, Shale Unit, Sandstone-Claystone Unit, Sandstone Unit, and also Alluvial Unit which is deposited unconformably on all of those rocks as the youngest unit. Shale Unit is deposited in laccustrine environment and is equalized to Sangkarewang Formation. Sandstone-Claystone Unit is deposited in meandering streams and is equalized to Sawahlunto Formation. Sandstone Unit is deposited in braided river system and is equalized to Sawahtambang Formation. The geological structures that developed in the area include fault structures that are represented by Tumpuktengah Strike Slip Fault, Parambahan Strike Slip Fault, Sarasah Strike Slip Fault, and Tanjung Ampalu Strike Slip Fault. 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 Morphology of this area is divided into four geomorphology units: Fold Hills Unit, Homoclinal Plain Unit, Intrusive Hills Unit is characterized by steep slopes and consists of granite, Alluvial Plain Unit is showed by plain morphology that lies alongside Buluhrotan River flow. The Stratigraphy of this area is divided into five illegitimate units of lithostratigraphy. The following are sorted from the oldest to the youngest, those are: Pre- Tertiary Granite Unit, Shale Unit, Sandstone-Claystone Unit, Sandstone Unit, and also Alluvial Unit which is deposited unconformably on all of those rocks as the youngest unit. Shale Unit is deposited in laccustrine environment and is equalized to Sangkarewang Formation. Sandstone-Claystone Unit is deposited in meandering streams and is equalized to Sawahlunto Formation. Sandstone Unit is deposited in braided river system and is equalized to Sawahtambang Formation. The geological structures that developed in the area include fault structures that are represented by Tumpuktengah Strike Slip Fault, Parambahan Strike Slip Fault, Sarasah Strike Slip Fault, and Tanjung Ampalu Strike Slip Fault.
format Final Project
author FERNANDO BUTARBUTAR (NIM 12007007), ELREY
spellingShingle FERNANDO BUTARBUTAR (NIM 12007007), ELREY
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author_facet FERNANDO BUTARBUTAR (NIM 12007007), ELREY
author_sort FERNANDO BUTARBUTAR (NIM 12007007), ELREY
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/13426
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