Geology and biogeochemical study in Sokor, Kelantan

Biogeochemistry is a multidisciplinary field that studies the complex relationship between geological and biological components. This research investigated the relationship of plants with ore elements in term of geochemistry and mineralogy. Geological mapping had been carried out: the identified lit...

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Main Author: Chang Shen Chang
Format: Undergraduate Final Project Report
Language:English
Published: 2019
Online Access:http://discol.umk.edu.my/id/eprint/4466/1/Chang%20Shen%20Chang.pdf
http://discol.umk.edu.my/id/eprint/4466/
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Institution: Universiti Malaysia Kelantan
Language: English
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spelling my.umk.eprints.44662022-05-23T22:12:17Z http://discol.umk.edu.my/id/eprint/4466/ Geology and biogeochemical study in Sokor, Kelantan Chang Shen Chang Biogeochemistry is a multidisciplinary field that studies the complex relationship between geological and biological components. This research investigated the relationship of plants with ore elements in term of geochemistry and mineralogy. Geological mapping had been carried out: the identified lithology of the study area with 25 kilometres squared is argillaceous and calcareous units and the geological structures of folding which contribute to the current bed dipping and hydrothermal alteration through joint infilling has indicated an ore deposit region. In preliminary study, seven sets of soil samples were collected and analysed through Atomic Absorption Spectrophotometer to scope down the study area. Four sets of soil and plant samples had been collected and characterized through Fourier-Transform InfraRed Spectroscopy, X-ray methods (X-Ray Diffraction and X-Ray Fluorescence) and Inductively Coupled Plasma Mass Spectrometry respectively. The main composition of soil is clay minerals, kaolinite, dickite and pyrophyliite which can indicate argillic alteration and possible supergene enrichment for ore deposition. Phyllic alteration has also been found in area close to the study area with mineral assemblage of pyrite, quartz and sericite. There is also a relationship between the geomorphology, plant morphology and the ore element content in the soil: metal elements concentration is higher in lower elevation except aluminium and iron; the differential morphology of Melastoma malabathricum can indicate iron concentration in the soil. The findings of this research will be useful for diversifying current mineral exploration method in general and providing database for further investigation in the study area in specific. 2019 Undergraduate Final Project Report NonPeerReviewed text en http://discol.umk.edu.my/id/eprint/4466/1/Chang%20Shen%20Chang.pdf Chang Shen Chang (2019) Geology and biogeochemical study in Sokor, Kelantan. 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 Biogeochemistry is a multidisciplinary field that studies the complex relationship between geological and biological components. This research investigated the relationship of plants with ore elements in term of geochemistry and mineralogy. Geological mapping had been carried out: the identified lithology of the study area with 25 kilometres squared is argillaceous and calcareous units and the geological structures of folding which contribute to the current bed dipping and hydrothermal alteration through joint infilling has indicated an ore deposit region. In preliminary study, seven sets of soil samples were collected and analysed through Atomic Absorption Spectrophotometer to scope down the study area. Four sets of soil and plant samples had been collected and characterized through Fourier-Transform InfraRed Spectroscopy, X-ray methods (X-Ray Diffraction and X-Ray Fluorescence) and Inductively Coupled Plasma Mass Spectrometry respectively. The main composition of soil is clay minerals, kaolinite, dickite and pyrophyliite which can indicate argillic alteration and possible supergene enrichment for ore deposition. Phyllic alteration has also been found in area close to the study area with mineral assemblage of pyrite, quartz and sericite. There is also a relationship between the geomorphology, plant morphology and the ore element content in the soil: metal elements concentration is higher in lower elevation except aluminium and iron; the differential morphology of Melastoma malabathricum can indicate iron concentration in the soil. The findings of this research will be useful for diversifying current mineral exploration method in general and providing database for further investigation in the study area in specific.
format Undergraduate Final Project Report
author Chang Shen Chang
spellingShingle Chang Shen Chang
Geology and biogeochemical study in Sokor, Kelantan
author_facet Chang Shen Chang
author_sort Chang Shen Chang
title Geology and biogeochemical study in Sokor, Kelantan
title_short Geology and biogeochemical study in Sokor, Kelantan
title_full Geology and biogeochemical study in Sokor, Kelantan
title_fullStr Geology and biogeochemical study in Sokor, Kelantan
title_full_unstemmed Geology and biogeochemical study in Sokor, Kelantan
title_sort geology and biogeochemical study in sokor, kelantan
publishDate 2019
url http://discol.umk.edu.my/id/eprint/4466/1/Chang%20Shen%20Chang.pdf
http://discol.umk.edu.my/id/eprint/4466/
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