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Geomorphology of research area consists of three geomorphology units: Anticline Valley Unit, Lava Dome Unit and Alluvial Plain Unit. Historical geology of research area starts from Middle Miocene Epoch while deposition of Claystone-Sandstone Unit in Middle Neritic environment, then regression and co...

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Main Author:	BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN
Format:	Final Project
Language:	Indonesia
Online Access:	https://digilib.itb.ac.id/gdl/view/14551
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Institution:	Institut Teknologi Bandung
Language:	Indonesia

id	id-itb.:14551
spelling	id-itb.:145512017-09-27T11:46:39Z#TITLE_ALTERNATIVE# BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/14551 Geomorphology of research area consists of three geomorphology units: Anticline Valley Unit, Lava Dome Unit and Alluvial Plain Unit. Historical geology of research area starts from Middle Miocene Epoch while deposition of Claystone-Sandstone Unit in Middle Neritic environment, then regression and continued conformably by deposition of Sandstone Unit in delta environment. This unit is depositioned at Late Miocene and contains coal intercalation. Plio-Pleistocene tectonic activity results deformation in research area such as Lematang Anticline and Kanti Fault. Andesite Unit is formed at Pleistocene in terrestrial environment and unconformably covers the older units. The younger unit in research area is Alluvial Unit and its deposition working until now. 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	Geomorphology of research area consists of three geomorphology units: Anticline Valley Unit, Lava Dome Unit and Alluvial Plain Unit. Historical geology of research area starts from Middle Miocene Epoch while deposition of Claystone-Sandstone Unit in Middle Neritic environment, then regression and continued conformably by deposition of Sandstone Unit in delta environment. This unit is depositioned at Late Miocene and contains coal intercalation. Plio-Pleistocene tectonic activity results deformation in research area such as Lematang Anticline and Kanti Fault. Andesite Unit is formed at Pleistocene in terrestrial environment and unconformably covers the older units. The younger unit in research area is Alluvial Unit and its deposition working until now.
format	Final Project
author	BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN
spellingShingle	BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN #TITLE_ALTERNATIVE#
author_facet	BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN
author_sort	BASTIAN PANGGABEAN (NIM 12006059); Pembimbing: Dr. Ir. Bambang Priadi, YAN
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/14551
_version_	1820737252553129984

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