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Geomorphology units in the area include Folded Mountain, Intrusion Ridge, and Alluvial Plan Units. There are seven informally rock units present, including Tuf-Sandstone, Limestone, Tuff-Sandstone Intercalated with Breccia, Polimic Breccia, Monomic Breccia, Andesite Intrusion, and Alluvial Units. Th...

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Main Author: ARI WIYOGA (NIM 12005017), SONNY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13846
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13846
spelling id-itb.:138462017-09-27T11:46:39Z#TITLE_ALTERNATIVE# ARI WIYOGA (NIM 12005017), SONNY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13846 Geomorphology units in the area include Folded Mountain, Intrusion Ridge, and Alluvial Plan Units. There are seven informally rock units present, including Tuf-Sandstone, Limestone, Tuff-Sandstone Intercalated with Breccia, Polimic Breccia, Monomic Breccia, Andesite Intrusion, and Alluvial Units. The geological structures developed in this area an E-W trend fold (sincline and anticline), a NNE-WSW trend strike slip fault and an inferred NNE-WSW trend normal fault (based on reconstruction of geology section). The development of the Limestone Unit of Citarate Formation from bottom to top are algae packstone, packstone-grainstone, coral-algae packstone, and foraminifer wackestone-packstone. Based on textures and faunal assemblages limestone of The Citarate Formation, algae packstone, coral-algae packstone, and foraminifer wackestone-packstone are interpreted to be deposited in an open platform backreef environment whereas packstone-grainstone is interpreted to be deposited in forereef environment (toe of slope and open sea shelf). 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 units in the area include Folded Mountain, Intrusion Ridge, and Alluvial Plan Units. There are seven informally rock units present, including Tuf-Sandstone, Limestone, Tuff-Sandstone Intercalated with Breccia, Polimic Breccia, Monomic Breccia, Andesite Intrusion, and Alluvial Units. The geological structures developed in this area an E-W trend fold (sincline and anticline), a NNE-WSW trend strike slip fault and an inferred NNE-WSW trend normal fault (based on reconstruction of geology section). The development of the Limestone Unit of Citarate Formation from bottom to top are algae packstone, packstone-grainstone, coral-algae packstone, and foraminifer wackestone-packstone. Based on textures and faunal assemblages limestone of The Citarate Formation, algae packstone, coral-algae packstone, and foraminifer wackestone-packstone are interpreted to be deposited in an open platform backreef environment whereas packstone-grainstone is interpreted to be deposited in forereef environment (toe of slope and open sea shelf).
format Final Project
author ARI WIYOGA (NIM 12005017), SONNY
spellingShingle ARI WIYOGA (NIM 12005017), SONNY
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author_facet ARI WIYOGA (NIM 12005017), SONNY
author_sort ARI WIYOGA (NIM 12005017), SONNY
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/13846
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