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Geology and Sedimentology of Paya Peda, Jertih

Paya Peda is a study area located in Jerteh, Terengganu The purpose of this research is to produce a geological map of Paya Peda, to identify species of ferns fossils found in the Paya Peda and to interpret the paleo-depositional environment of Paya Pedal were three methods used inthis reseach.Among...

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Main Author: Nor Fatimah Kamarudin
Format: Undergraduate Final Project Report
Published: 2015
Online Access:http://discol.umk.edu.my/id/eprint/6286/
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spelling my.umk.eprints.62862022-05-23T08:46:17Z http://discol.umk.edu.my/id/eprint/6286/ Geology and Sedimentology of Paya Peda, Jertih Nor Fatimah Kamarudin Paya Peda is a study area located in Jerteh, Terengganu The purpose of this research is to produce a geological map of Paya Peda, to identify species of ferns fossils found in the Paya Peda and to interpret the paleo-depositional environment of Paya Pedal were three methods used inthis reseach.Among the methods used includes petrographic analysis, structural analysis and fades analysis. From the study, Paya Peda can be categorised in the Telemong Formation of Carboniferous age consisting of several types rock such as interbedded shale and mudstone and alluvium lithology. Cordaites sp., Pecopteris sp., Neoropteris sp., and Sigillaria sp. were among four species have been identified in the area of Paya Peda.Interpretation of depositional environment suggests that the mudstone and shale deposited under the low energy current environment. Besides that, the fern fossils give the indication that Paya Peda surrounding area is a humid climate area according to an adaptation of ferns habitat. So it can be concluded that the Paya Peda deposited in the , paludal (swamp) environment which has a high carbon content. 2015 Undergraduate Final Project Report NonPeerReviewed Nor Fatimah Kamarudin (2015) Geology and Sedimentology of Paya Peda, Jertih. Undergraduate Final Project Report thesis, Faculty of Earth Science. (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 Paya Peda is a study area located in Jerteh, Terengganu The purpose of this research is to produce a geological map of Paya Peda, to identify species of ferns fossils found in the Paya Peda and to interpret the paleo-depositional environment of Paya Pedal were three methods used inthis reseach.Among the methods used includes petrographic analysis, structural analysis and fades analysis. From the study, Paya Peda can be categorised in the Telemong Formation of Carboniferous age consisting of several types rock such as interbedded shale and mudstone and alluvium lithology. Cordaites sp., Pecopteris sp., Neoropteris sp., and Sigillaria sp. were among four species have been identified in the area of Paya Peda.Interpretation of depositional environment suggests that the mudstone and shale deposited under the low energy current environment. Besides that, the fern fossils give the indication that Paya Peda surrounding area is a humid climate area according to an adaptation of ferns habitat. So it can be concluded that the Paya Peda deposited in the , paludal (swamp) environment which has a high carbon content.
format Undergraduate Final Project Report
author Nor Fatimah Kamarudin
spellingShingle Nor Fatimah Kamarudin
Geology and Sedimentology of Paya Peda, Jertih
author_facet Nor Fatimah Kamarudin
author_sort Nor Fatimah Kamarudin
title Geology and Sedimentology of Paya Peda, Jertih
title_short Geology and Sedimentology of Paya Peda, Jertih
title_full Geology and Sedimentology of Paya Peda, Jertih
title_fullStr Geology and Sedimentology of Paya Peda, Jertih
title_full_unstemmed Geology and Sedimentology of Paya Peda, Jertih
title_sort geology and sedimentology of paya peda, jertih
publishDate 2015
url http://discol.umk.edu.my/id/eprint/6286/
_version_ 1763303674828816384
score 13.211869

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