Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia

Organic-rich shales occur in the Kockatea Shale Formation, Permo-Triassic of the Perth Basin (Western Australia) and have been investigated to characterise it as a potential shale gas unit. Classic sedimentological investigation methods, including core descriptions and thin section microscopy, were...

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Main Authors: Torghabeh, A., Rezaee, M. Reza, Moussavi-Harami, R., Pimentel, N.
Format: Journal Article
Published: Inder Science Publishers 2014
Online Access:http://hdl.handle.net/20.500.11937/10893
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author Torghabeh, A.
Rezaee, M. Reza
Moussavi-Harami, R.
Pimentel, N.
author_facet Torghabeh, A.
Rezaee, M. Reza
Moussavi-Harami, R.
Pimentel, N.
author_sort Torghabeh, A.
building Curtin Institutional Repository
collection Online Access
description Organic-rich shales occur in the Kockatea Shale Formation, Permo-Triassic of the Perth Basin (Western Australia) and have been investigated to characterise it as a potential shale gas unit. Classic sedimentological investigation methods, including core descriptions and thin section microscopy, were coupled with standardised organic geochemical analysis procedures, such as TOC determination and Rock-Eval pyrolysis, as well as maceral composition analysis and vitrinite reflectance (Ro) measurements. The Kockatea sediments show a trend of increasing maturity from north to south, with Ro values ranging from 0.6 to 2%, pointing to a thermal maturity between the wet and dry thermogenic gas window. The organic matter is a mixed Type II/III kerogen and hydrogen index (HI) values range from 0.1 to 662 mg HC/g rock, with total organic carbon (TOC) contents between 0.02 and 12.64 wt% and an average formation thickness of 337 m. These interdisciplinary data and methods point to a good potential of the Kockatea Shale Formation for shale gas exploration in Western Australia.
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spelling curtin-20.500.11937-108932017-09-13T14:55:04Z Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia Torghabeh, A. Rezaee, M. Reza Moussavi-Harami, R. Pimentel, N. Organic-rich shales occur in the Kockatea Shale Formation, Permo-Triassic of the Perth Basin (Western Australia) and have been investigated to characterise it as a potential shale gas unit. Classic sedimentological investigation methods, including core descriptions and thin section microscopy, were coupled with standardised organic geochemical analysis procedures, such as TOC determination and Rock-Eval pyrolysis, as well as maceral composition analysis and vitrinite reflectance (Ro) measurements. The Kockatea sediments show a trend of increasing maturity from north to south, with Ro values ranging from 0.6 to 2%, pointing to a thermal maturity between the wet and dry thermogenic gas window. The organic matter is a mixed Type II/III kerogen and hydrogen index (HI) values range from 0.1 to 662 mg HC/g rock, with total organic carbon (TOC) contents between 0.02 and 12.64 wt% and an average formation thickness of 337 m. These interdisciplinary data and methods point to a good potential of the Kockatea Shale Formation for shale gas exploration in Western Australia. 2014 Journal Article http://hdl.handle.net/20.500.11937/10893 10.1504/IJOGCT.2014.064420 Inder Science Publishers restricted
spellingShingle Torghabeh, A.
Rezaee, M. Reza
Moussavi-Harami, R.
Pimentel, N.
Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title_full Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title_fullStr Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title_full_unstemmed Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title_short Unconventional resource evaluation: Kockatea shale, Perth basin, Western Australia
title_sort unconventional resource evaluation: kockatea shale, perth basin, western australia
url http://hdl.handle.net/20.500.11937/10893