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Stratigraphy units in research area consist of Sandstone A, Claystone, Sandstone B, Claystone - Sandstone, and Alluvium Units. Research of sedimentary structure of stratigraphy units in research area show some parallel lamination and cross lamination/cross bedding that specifically found in fluviati...

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Main Author:	RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY
Format:	Final Project
Language:	Indonesia
Online Access:	https://digilib.itb.ac.id/gdl/view/13355
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Institution:	Institut Teknologi Bandung
Language:	Indonesia

id	id-itb.:13355
spelling	id-itb.:133552017-09-27T11:46:40Z#TITLE_ALTERNATIVE# RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13355 Stratigraphy units in research area consist of Sandstone A, Claystone, Sandstone B, Claystone - Sandstone, and Alluvium Units. Research of sedimentary structure of stratigraphy units in research area show some parallel lamination and cross lamination/cross bedding that specifically found in fluviatil depositional environments also some flaser that show a transition depositional environment. That stratigraphy units equal with two formation, Tabul Formation in Late Miocene and Meliat Formation in Middle Miocene.<p>Structures in research area show NE-SW and NW-SE direction. This direction representation strike slip fault. Strike slip fault in research area consist of dextral strike slip fault (Tabur Fault) and sinistral strike slip fault (Seimenggaris Fault and Bukit Datuk 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	Stratigraphy units in research area consist of Sandstone A, Claystone, Sandstone B, Claystone - Sandstone, and Alluvium Units. Research of sedimentary structure of stratigraphy units in research area show some parallel lamination and cross lamination/cross bedding that specifically found in fluviatil depositional environments also some flaser that show a transition depositional environment. That stratigraphy units equal with two formation, Tabul Formation in Late Miocene and Meliat Formation in Middle Miocene.<p>Structures in research area show NE-SW and NW-SE direction. This direction representation strike slip fault. Strike slip fault in research area consist of dextral strike slip fault (Tabur Fault) and sinistral strike slip fault (Seimenggaris Fault and Bukit Datuk Fault).
format	Final Project
author	RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY
spellingShingle	RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY #TITLE_ALTERNATIVE#
author_facet	RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY
author_sort	RIEZA AULIANDRI (NIM 12006032); Pembimbing: Dr.Ir. Chalid Idham Abdullah dan Ir. Benyamin Sapi, DANDY
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/13355
_version_	1820736162519580672

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