The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H)

M Ladjavadi; K Grice; D Edwards; C Boreham; Ian Metcalfe; R Summons

Abstract

The Perth Basin petroleum system has been intermittently explored for the last few decades, resulting in the production of gas and oil from several onshore fields. The effective source rock for petroleum in the Perth Basin is the marine Kockatea Shale, with the hydrogen-richest interval being the Sapropelic Unit of the Hovea Member. The Perth Basin in southwest Western Australia (WA) is a deep, north to south trending basin. The Perth Basin sediments comprise of rocks of Permian-Early Cretaceous in age. The current perception is that the area is gas prone and has been challenged with the recent discovery of the near-shore Cliff Head oil field. The Dongara gas field in the onshore Perth Basin contains more than half the oil and gas reserves. The Perth Basin sediments used in this study are from Senecio-1 core which is located approximately 15.5km from the north of Dongara.

Original language	English
Pages	83-83
Publication status	Published - 2011
Event	ICCP 2011: XVII International Congress on the Carboniferous and Permian - Perth, Australia Duration: 3 Jul 2011 → 8 Jul 2011

Conference

Conference	ICCP 2011: XVII International Congress on the Carboniferous and Permian
City	Perth, Australia
Period	3/07/11 → 8/07/11

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 14 Life Below Water

Keywords

Organic Geochemistry

Access to Document

https://hdl.handle.net/1959.11/8407

Handle.net

Persistent link

Cite this

Ladjavadi, M., Grice, K., Edwards, D., Boreham, C., Metcalfe, I., & Summons, R. (2011). The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H). 83-83. Abstract from ICCP 2011: XVII International Congress on the Carboniferous and Permian, Perth, Australia. https://hdl.handle.net/1959.11/8407

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title = "The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H)",

abstract = "The Perth Basin petroleum system has been intermittently explored for the last few decades, resulting in the production of gas and oil from several onshore fields. The effective source rock for petroleum in the Perth Basin is the marine Kockatea Shale, with the hydrogen-richest interval being the Sapropelic Unit of the Hovea Member. The Perth Basin in southwest Western Australia (WA) is a deep, north to south trending basin. The Perth Basin sediments comprise of rocks of Permian-Early Cretaceous in age. The current perception is that the area is gas prone and has been challenged with the recent discovery of the near-shore Cliff Head oil field. The Dongara gas field in the onshore Perth Basin contains more than half the oil and gas reserves. The Perth Basin sediments used in this study are from Senecio-1 core which is located approximately 15.5km from the north of Dongara.",

keywords = "Organic Geochemistry",

author = "M Ladjavadi and K Grice and D Edwards and C Boreham and Ian Metcalfe and R Summons",

year = "2011",

language = "English",

pages = "83--83",

note = "ICCP 2011: XVII International Congress on the Carboniferous and Permian ; Conference date: 03-07-2011 Through 08-07-2011",

}

Ladjavadi, M, Grice, K, Edwards, D, Boreham, C, Metcalfe, I & Summons, R 2011, 'The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H)', ICCP 2011: XVII International Congress on the Carboniferous and Permian, Perth, Australia, 3/07/11 - 8/07/11 pp. 83-83. <https://hdl.handle.net/1959.11/8407>

The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H). / Ladjavadi, M; Grice, K; Edwards, D et al.
2011. 83-83 Abstract from ICCP 2011: XVII International Congress on the Carboniferous and Permian, Perth, Australia.

Research output: Contribution to conference › Abstract

TY - CONF

T1 - The age and palaeoenvironmental conditions spanning the Permian/Triassic boundary in the northern onshore Perth Basin by using biomarker distributions and stable isotopes (C, H)

AU - Ladjavadi, M

AU - Grice, K

AU - Edwards, D

AU - Boreham, C

AU - Metcalfe, Ian

AU - Summons, R

PY - 2011

Y1 - 2011

N2 - The Perth Basin petroleum system has been intermittently explored for the last few decades, resulting in the production of gas and oil from several onshore fields. The effective source rock for petroleum in the Perth Basin is the marine Kockatea Shale, with the hydrogen-richest interval being the Sapropelic Unit of the Hovea Member. The Perth Basin in southwest Western Australia (WA) is a deep, north to south trending basin. The Perth Basin sediments comprise of rocks of Permian-Early Cretaceous in age. The current perception is that the area is gas prone and has been challenged with the recent discovery of the near-shore Cliff Head oil field. The Dongara gas field in the onshore Perth Basin contains more than half the oil and gas reserves. The Perth Basin sediments used in this study are from Senecio-1 core which is located approximately 15.5km from the north of Dongara.

AB - The Perth Basin petroleum system has been intermittently explored for the last few decades, resulting in the production of gas and oil from several onshore fields. The effective source rock for petroleum in the Perth Basin is the marine Kockatea Shale, with the hydrogen-richest interval being the Sapropelic Unit of the Hovea Member. The Perth Basin in southwest Western Australia (WA) is a deep, north to south trending basin. The Perth Basin sediments comprise of rocks of Permian-Early Cretaceous in age. The current perception is that the area is gas prone and has been challenged with the recent discovery of the near-shore Cliff Head oil field. The Dongara gas field in the onshore Perth Basin contains more than half the oil and gas reserves. The Perth Basin sediments used in this study are from Senecio-1 core which is located approximately 15.5km from the north of Dongara.

KW - Organic Geochemistry

UR - http://geodocs.doir.wa.gov.au/search.jsp?cabinetId=1101&Combined=N11X

UR - http://trove.nla.gov.au/work/155774845

M3 - Abstract

SP - 83

EP - 83

T2 - ICCP 2011: XVII International Congress on the Carboniferous and Permian

Y2 - 3 July 2011 through 8 July 2011

ER -