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Based on regional fisiography in Easterm part of Central Java, research area is located in Kendeng Zone and Solo Zone. Study area is divided into 2 geomorphology units which are Ridge Homoklin and Aluvial Plains. Stratigraphy unit in study area divided into 4 unofficial lithology unit from oldest to...

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Main Author: SATYA DEWI (NIM 12007051), YANUARIA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/13910
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:13910
spelling id-itb.:139102017-09-27T11:46:39Z#TITLE_ALTERNATIVE# SATYA DEWI (NIM 12007051), YANUARIA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13910 Based on regional fisiography in Easterm part of Central Java, research area is located in Kendeng Zone and Solo Zone. Study area is divided into 2 geomorphology units which are Ridge Homoklin and Aluvial Plains. Stratigraphy unit in study area divided into 4 unofficial lithology unit from oldest to youngest lithology units. Marl-Limestone Unit which was deposited in Late Miocene and then Marl-Sandstone was deposited above it in early Pliocene, Limestone unit was deposited in Pliocene and wedges with Marl-Sandstone unit. In Post Pliocene, tectonic activity occured and caused layer has dip, fault and uplift, then erosion occured and caused geomorphology forming. In Recent, Aluvial Unit was deposited. Structure geology which appears in study area is intrepretation strike-slip fault that is Strike Slip Fault Tangen, Strike Slip Fault Katelan and Strike Slip Fault Dunggringan. 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 Based on regional fisiography in Easterm part of Central Java, research area is located in Kendeng Zone and Solo Zone. Study area is divided into 2 geomorphology units which are Ridge Homoklin and Aluvial Plains. Stratigraphy unit in study area divided into 4 unofficial lithology unit from oldest to youngest lithology units. Marl-Limestone Unit which was deposited in Late Miocene and then Marl-Sandstone was deposited above it in early Pliocene, Limestone unit was deposited in Pliocene and wedges with Marl-Sandstone unit. In Post Pliocene, tectonic activity occured and caused layer has dip, fault and uplift, then erosion occured and caused geomorphology forming. In Recent, Aluvial Unit was deposited. Structure geology which appears in study area is intrepretation strike-slip fault that is Strike Slip Fault Tangen, Strike Slip Fault Katelan and Strike Slip Fault Dunggringan.
format Final Project
author SATYA DEWI (NIM 12007051), YANUARIA
spellingShingle SATYA DEWI (NIM 12007051), YANUARIA
#TITLE_ALTERNATIVE#
author_facet SATYA DEWI (NIM 12007051), YANUARIA
author_sort SATYA DEWI (NIM 12007051), YANUARIA
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/13910
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