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Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products

A geological study is conducted in Kp.Cipeuteuy, Bandung West Java with an area of 25km2 and contour interval of 12.5 meters. The area is located in Kabupaten Bandung, geographically in 107 °35′45.03” - 107 °38’30.06” East-longitude, and 7°1′53.00 - 7°4'37.38” on South-latitude. This study a...

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Main Author: Naziha Nordin
Format: Undergraduate Final Project Report
Language:English
Published: 2019
Online Access:http://discol.umk.edu.my/id/eprint/4622/1/Naziha%20Binti%20Nordin.pdf
http://discol.umk.edu.my/id/eprint/4622/
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spelling my.umk.eprints.46222022-05-23T21:11:23Z http://discol.umk.edu.my/id/eprint/4622/ Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products Naziha Nordin A geological study is conducted in Kp.Cipeuteuy, Bandung West Java with an area of 25km2 and contour interval of 12.5 meters. The area is located in Kabupaten Bandung, geographically in 107 °35′45.03” - 107 °38’30.06” East-longitude, and 7°1′53.00 - 7°4'37.38” on South-latitude. This study aims to produce a geological map of 1:25,000 scale and specify in petrogenesis and evolution of magma based on the volcanic products in the study area. The evolution and genesis of volcanic products is studied and supported with thin section and detection of major and trace elements using X-Ray Fluorescent (XRF). The result is analysed through few plotting made based on Streckeisen, (1973), Mullen (1983), Peccerillo and Taylor, (1976), Le Bas et.al, (1986), and Harker’s diagram for major and trace elements. Stratigraphically, the study area has occurred few series of eruptions happened continuously in the period of Late Miocene and Pleistocene. The oldest rock is Tan, andesite with composition of plagioclase and pyroxene. Tan is pillowing Ԛan and Ql, series of andesite with composition of plagioclase, pyroxene and hornblende that interfingering with each other due to the age gap happened in volcanic eruptions. The youngest lies on top of Qan and Ql are Qvb which is volcanic breccia, a monomict type of breccia, with component of andesite and tuff as matrix. Qvb is interfingered with Qt, which is crystal-dominated tuff. The genesis of magma is in the island arc with calc-alkaline series. The geological map and geochemical analysis will provide additional and updated data for the use of future scientific research. 2019 Undergraduate Final Project Report NonPeerReviewed text en http://discol.umk.edu.my/id/eprint/4622/1/Naziha%20Binti%20Nordin.pdf Naziha Nordin (2019) Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products. 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/
language English
description A geological study is conducted in Kp.Cipeuteuy, Bandung West Java with an area of 25km2 and contour interval of 12.5 meters. The area is located in Kabupaten Bandung, geographically in 107 °35′45.03” - 107 °38’30.06” East-longitude, and 7°1′53.00 - 7°4'37.38” on South-latitude. This study aims to produce a geological map of 1:25,000 scale and specify in petrogenesis and evolution of magma based on the volcanic products in the study area. The evolution and genesis of volcanic products is studied and supported with thin section and detection of major and trace elements using X-Ray Fluorescent (XRF). The result is analysed through few plotting made based on Streckeisen, (1973), Mullen (1983), Peccerillo and Taylor, (1976), Le Bas et.al, (1986), and Harker’s diagram for major and trace elements. Stratigraphically, the study area has occurred few series of eruptions happened continuously in the period of Late Miocene and Pleistocene. The oldest rock is Tan, andesite with composition of plagioclase and pyroxene. Tan is pillowing Ԛan and Ql, series of andesite with composition of plagioclase, pyroxene and hornblende that interfingering with each other due to the age gap happened in volcanic eruptions. The youngest lies on top of Qan and Ql are Qvb which is volcanic breccia, a monomict type of breccia, with component of andesite and tuff as matrix. Qvb is interfingered with Qt, which is crystal-dominated tuff. The genesis of magma is in the island arc with calc-alkaline series. The geological map and geochemical analysis will provide additional and updated data for the use of future scientific research.
format Undergraduate Final Project Report
author Naziha Nordin
spellingShingle Naziha Nordin
Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
author_facet Naziha Nordin
author_sort Naziha Nordin
title Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
title_short Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
title_full Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
title_fullStr Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
title_full_unstemmed Geology of Kp.Cipeuteuy, Bandung West Java and petrology of its volcanic products
title_sort geology of kp.cipeuteuy, bandung west java and petrology of its volcanic products
publishDate 2019
url http://discol.umk.edu.my/id/eprint/4622/1/Naziha%20Binti%20Nordin.pdf
http://discol.umk.edu.my/id/eprint/4622/
_version_ 1763303439829303296
score 13.211869

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