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Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia

The study area is located in the Nglanggeran district, Gunung Kidul Regency, Special Province of Yogyakarta that was located at the Southern Mountain along the southern part of Jawa Island in Indonesia. This research paper is concern with the objectives of updating the geological map in the scale of...

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Main Author: 'Aqilah Anuar
Format: Undergraduate Final Project Report
Published: 2018
Online Access:http://discol.umk.edu.my/id/eprint/4881/
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spelling my.umk.eprints.48812022-07-03T03:01:51Z http://discol.umk.edu.my/id/eprint/4881/ Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia 'Aqilah Anuar The study area is located in the Nglanggeran district, Gunung Kidul Regency, Special Province of Yogyakarta that was located at the Southern Mountain along the southern part of Jawa Island in Indonesia. This research paper is concern with the objectives of updating the geological map in the scale of l :25,000 and to study the facies association for interpreting the depositional environment of the Sambipitu Formation, which is one of the formations lies in the study area. The methodology that was done throughout the project is by the remote sensing interpretation, fieldworks and laboratory works. Stratigraphically, there are four formations deposited in the study area. There are the Nglanggeran, overlain by the Sambipitu, the Oyo and the Wonosari Formation respectively. All of the formations have distinct characteristics based on lithologies and morphologies. The stratigraphic section was carried out along the Ngalang River to establish the parameters needed for interpreting the depositional environment. The parameters used are facies associations, sedimentary structures and ichnofossils. Based on the dominant sandstones and mudstones, and the sedimentary structures of lenticular bedding, wavy bedding, normal grading, cross beddings, parallel lamination, slumps and convolute bedding, the depositional environment of the Sambipitu Formation is interpreted to be in the shallow marine. The interpretation is supported by the presence of ichnofossils from the Skolithos and Cruziana ichnofacies which can be found within the shallow marine environment. 2018 Undergraduate Final Project Report NonPeerReviewed 'Aqilah Anuar (2018) Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia. Final Year Project thesis, Universiti Malaysia Kelantan. (Submitted)
institution Universiti Malaysia Kelantan
building Perpustakaan Universiti Malaysia Kelantan
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Kelantan
content_source UMK Institutional Repository
url_provider http://umkeprints.umk.edu.my/
description The study area is located in the Nglanggeran district, Gunung Kidul Regency, Special Province of Yogyakarta that was located at the Southern Mountain along the southern part of Jawa Island in Indonesia. This research paper is concern with the objectives of updating the geological map in the scale of l :25,000 and to study the facies association for interpreting the depositional environment of the Sambipitu Formation, which is one of the formations lies in the study area. The methodology that was done throughout the project is by the remote sensing interpretation, fieldworks and laboratory works. Stratigraphically, there are four formations deposited in the study area. There are the Nglanggeran, overlain by the Sambipitu, the Oyo and the Wonosari Formation respectively. All of the formations have distinct characteristics based on lithologies and morphologies. The stratigraphic section was carried out along the Ngalang River to establish the parameters needed for interpreting the depositional environment. The parameters used are facies associations, sedimentary structures and ichnofossils. Based on the dominant sandstones and mudstones, and the sedimentary structures of lenticular bedding, wavy bedding, normal grading, cross beddings, parallel lamination, slumps and convolute bedding, the depositional environment of the Sambipitu Formation is interpreted to be in the shallow marine. The interpretation is supported by the presence of ichnofossils from the Skolithos and Cruziana ichnofacies which can be found within the shallow marine environment.
format Undergraduate Final Project Report
author 'Aqilah Anuar
spellingShingle 'Aqilah Anuar
Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
author_facet 'Aqilah Anuar
author_sort 'Aqilah Anuar
title Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
title_short Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
title_full Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
title_fullStr Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
title_full_unstemmed Geology and depositional environment of Sambipitu area, Nglanggeran district, Gunung Kidul regency, special province of Yogyakarta, Indonesia
title_sort geology and depositional environment of sambipitu area, nglanggeran district, gunung kidul regency, special province of yogyakarta, indonesia
publishDate 2018
url http://discol.umk.edu.my/id/eprint/4881/
_version_ 1763303475990495232
score 13.211869

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