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Appraisal and development of the Taq Taq field, Kurdistan region, Iraq

By
C. R. Garland
C. R. Garland
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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I. Abalioglu
I. Abalioglu
Taq Taq Operating Company Limited, Via Tower Bestepeler Mahallesi, Nergiz Sokak No 7/52, Sogutozu Ankara, Turkey
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L. Akca
L. Akca
Genel Enerji AS, Via Tower Bestepeler Mahallesi, Nergiz Sokak No 7/8, Sogutozu Ankara, Turkey
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A. Cassidy
A. Cassidy
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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Y. Chiffoleau
Y. Chiffoleau
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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L. Godail
L. Godail
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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M. A. S. Grace
M. A. S. Grace
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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H. J. Kader
H. J. Kader
Taq Taq Operating Company Limited, Via Tower Bestepeler Mahallesi, Nergiz Sokak No 7/52, Sogutozu Ankara, Turkey
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F. Khalek
F. Khalek
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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H. Legarre
H. Legarre
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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H. B. Nazhat
H. B. Nazhat
Kurdistan Regional Government-IRAQ, Council of Ministers, Ministry of Natural Resources
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B. Sallier
B. Sallier
Addax Petroleum Services and Sinopec, 16 Avenue Eugène-Pittard, CH1211, Geneva, Switzerland (e-mail: chris.garland@addaxpetroleum.com)
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Published:
January 01, 2010

Abstract

The Taq Taq Field is located within an anticline in the gently folded zone of the Zagros mountains, northeastern Iraq, approximately 50 km ESE of Erbil. The main reservoirs are fractured limestones and dolomites of Late Cretaceous age, with an oil column exceeding 500 m in thickness. Eocene limestones and dolomites at shallow depth form a subsidiary reservoir. The structure is a gentle thrust-related fold which has also been affected by dextral transpression. A pervasive fracture system is present within the reservoirs, giving good connectivity and deliverability. Initial discovery and appraisal was made in 1978 when three wells were drilled. The recent appraisal programme started in 2005 and by the end of 2008 two seismic surveys had been acquired and eight additional wells had been drilled. Mapping has incorporated a seismic principal component analysis for horizon and lithology identification. Modelling of the fractures has utilized a comprehensive data set derived from core and image logs. Special core analysis has been directed towards the understanding of the pore system and its interaction with the fractures. Synthesis of all these elements is performed in a dual-media dynamic model which is currently in use for development planning.

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Contents

Geological Society, London, Petroleum Geology Conference series

Petroleum Geology: From Mature Basins to New Frontiers – Proceedings of the 7th Petroleum Geology Conference

B. A. Vining
B. A. Vining
Baker Hughes, UK
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S. C. Pickering
S. C. Pickering
Schlumberger, Gatwick, UK
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Geological Society of London
Volume
7
ISBN electronic:
9781862394131
Publication date:
January 01, 2010

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