Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield

Tertiary coal from Merit-Pila coalfield, Central Sarawak, Malaysia were analysed their regional ranks and petroleum generative potential. Total organic carbon contents (TOC) of coals range from 18.1 to 71.4 wt. % and S2 values coal are range from 0.57 to 5.48 these shows that this coal really hav...

Full description

Saved in:
Bibliographic Details
Main Author: bin Md. Nor , Mohamad Hanif
Format: Final Year Project
Language:English
Published: Universiti Teknologi PETRONAS 2016
Subjects:
Online Access:http://utpedia.utp.edu.my/18198/1/DISSERTATION_MOHAMAD_HANIF_B_MD_NOR_18570_PETROLEUM_GEOSCIENCE_.PDF
http://utpedia.utp.edu.my/18198/
Tags: Add Tag
No Tags, Be the first to tag this record!
id my-utp-utpedia.18198
record_format eprints
spelling my-utp-utpedia.181982018-11-22T14:40:03Z http://utpedia.utp.edu.my/18198/ Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield bin Md. Nor , Mohamad Hanif G Geography (General) Tertiary coal from Merit-Pila coalfield, Central Sarawak, Malaysia were analysed their regional ranks and petroleum generative potential. Total organic carbon contents (TOC) of coals range from 18.1 to 71.4 wt. % and S2 values coal are range from 0.57 to 5.48 these shows that this coal really have high potential to be a source rock potential. The hydrogen index value ranging from 166 to 1069 mg HC/g, this indicate that these coal are dominated by type III kerogen and are thus considered to be generated mainly gas-prone and limited oil-prone. This is supported by the presence of significant amount (35-65% by volume) of gas prone vitrinite maceral. Vitrinite is among the most common of gas-prone macerals in coal. The Thermal Alteration index (TAI) also shows that these coal are an immature coal and only can produced mainly gas and a limited amount of oil. This is supported by the Tmax values ranges from 348 to 423 °C which shows that these coal are immature. Although these coal from Merit-Pila coalfield have a high potential to be source rock potential but the hydrogen index value shows that it only can generated mainly gas and limited oil and supported by the vitrinite maceral is dominated in the coal. The coal also immature to generate oil from the thermal alteration index supported by the Tmax value. Universiti Teknologi PETRONAS 2016-01 Final Year Project NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/18198/1/DISSERTATION_MOHAMAD_HANIF_B_MD_NOR_18570_PETROLEUM_GEOSCIENCE_.PDF bin Md. Nor , Mohamad Hanif (2016) Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield. Universiti Teknologi PETRONAS. (Submitted)
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Electronic and Digitized Intellectual Asset
url_provider http://utpedia.utp.edu.my/
language English
topic G Geography (General)
spellingShingle G Geography (General)
bin Md. Nor , Mohamad Hanif
Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
description Tertiary coal from Merit-Pila coalfield, Central Sarawak, Malaysia were analysed their regional ranks and petroleum generative potential. Total organic carbon contents (TOC) of coals range from 18.1 to 71.4 wt. % and S2 values coal are range from 0.57 to 5.48 these shows that this coal really have high potential to be a source rock potential. The hydrogen index value ranging from 166 to 1069 mg HC/g, this indicate that these coal are dominated by type III kerogen and are thus considered to be generated mainly gas-prone and limited oil-prone. This is supported by the presence of significant amount (35-65% by volume) of gas prone vitrinite maceral. Vitrinite is among the most common of gas-prone macerals in coal. The Thermal Alteration index (TAI) also shows that these coal are an immature coal and only can produced mainly gas and a limited amount of oil. This is supported by the Tmax values ranges from 348 to 423 °C which shows that these coal are immature. Although these coal from Merit-Pila coalfield have a high potential to be source rock potential but the hydrogen index value shows that it only can generated mainly gas and limited oil and supported by the vitrinite maceral is dominated in the coal. The coal also immature to generate oil from the thermal alteration index supported by the Tmax value.
format Final Year Project
author bin Md. Nor , Mohamad Hanif
author_facet bin Md. Nor , Mohamad Hanif
author_sort bin Md. Nor , Mohamad Hanif
title Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
title_short Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
title_full Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
title_fullStr Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
title_full_unstemmed Coal Petrology and Geochemistry of Upper Coal Zones and Lower Coal Zones of Nyalau Formation from Merit-Pila Coalfield
title_sort coal petrology and geochemistry of upper coal zones and lower coal zones of nyalau formation from merit-pila coalfield
publisher Universiti Teknologi PETRONAS
publishDate 2016
url http://utpedia.utp.edu.my/18198/1/DISSERTATION_MOHAMAD_HANIF_B_MD_NOR_18570_PETROLEUM_GEOSCIENCE_.PDF
http://utpedia.utp.edu.my/18198/
_version_ 1739832473679822848
score 13.160551