Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)

How subsurface anticlines (oil fields) link structurally with faults is of great relevance in the exploration and development of oil fields. In this context, we investigate the geometric relation between lower Balarud (LBR), upper Balarud (UBR) and Qaleh Nar (QN) subsurface anticlines that are the m...

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Main Authors: Ahmad Radmehr, Soumyajit Mukherjee, Mohammad Seraj, Raana Razavi Pash
Format: Article
Language:English
Published: General Directorate of Mineral Research and Exploration 2024-08-01
Series:Bulletin of the Mineral Research and Exploration
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Online Access:https://dergipark.org.tr/tr/download/article-file/3337944
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author Ahmad Radmehr
Soumyajit Mukherjee
Mohammad Seraj
Raana Razavi Pash
author_facet Ahmad Radmehr
Soumyajit Mukherjee
Mohammad Seraj
Raana Razavi Pash
author_sort Ahmad Radmehr
collection DOAJ
description How subsurface anticlines (oil fields) link structurally with faults is of great relevance in the exploration and development of oil fields. In this context, we investigate the geometric relation between lower Balarud (LBR), upper Balarud (UBR) and Qaleh Nar (QN) subsurface anticlines that are the main oil fields in the Northern Dezful Embayment, central Zagros. The Asmari (As) and the Bangestan (Bng) reservoirs are studied geophysically using seismic profiles, well data and underground contour maps (UGC). Interpretation of 3500 m deep seismic profiles indicates the geometry of the studied subsurface anticlines differs vertically and horizontally to a significant proportion. The interpreted structures much resemble As and Bng horizons in each anticline. The UBR got overturned on the LBR due to thrusting possibly in the Late Miocene. The LBR, like a rabbit-ear structure, is situated at the northern edge of the QN. The lower and upper Chenareh and LBR and UBR resemble structurally and are separated mutually by a steep (strike-slip) fault. The fault separates the LBR and UBR from the QN. Interaction of different factors: change in overburden pressure, rate of deformation and uplift in the different parts of the subsurface anticlines moved and accumulated Gachsaran Formationtowards both limbs of the anticlines.
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publisher General Directorate of Mineral Research and Exploration
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spelling doaj-art-75f30ac55fba4cd9b0fe02763dafe8c82025-08-20T02:12:37ZengGeneral Directorate of Mineral Research and ExplorationBulletin of the Mineral Research and Exploration0026-45632024-08-01174174678310.19111/bulletinofmre.134443376Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)Ahmad Radmehr0https://orcid.org/0000-0001-6469-0395Soumyajit Mukherjee1https://orcid.org/0000-0003-1600-4690Mohammad Seraj2https://orcid.org/0000-0003-1456-909XRaana Razavi Pash3https://orcid.org/0000-0001-7933-158XGeophysicist, National Iranian South Oil Company (NISOC), Ahwaz, IRANDepartment of Earth Sciences, Indian Institute of Technology Bombay, Mumbai, 400 076, Maharashtra, INDIAStructural geologist, National Iranian South Oil Company (NISOC), Ahwaz, IRANFcaulty of Earth Sciences, Shiraz University, Shiraz, IRANHow subsurface anticlines (oil fields) link structurally with faults is of great relevance in the exploration and development of oil fields. In this context, we investigate the geometric relation between lower Balarud (LBR), upper Balarud (UBR) and Qaleh Nar (QN) subsurface anticlines that are the main oil fields in the Northern Dezful Embayment, central Zagros. The Asmari (As) and the Bangestan (Bng) reservoirs are studied geophysically using seismic profiles, well data and underground contour maps (UGC). Interpretation of 3500 m deep seismic profiles indicates the geometry of the studied subsurface anticlines differs vertically and horizontally to a significant proportion. The interpreted structures much resemble As and Bng horizons in each anticline. The UBR got overturned on the LBR due to thrusting possibly in the Late Miocene. The LBR, like a rabbit-ear structure, is situated at the northern edge of the QN. The lower and upper Chenareh and LBR and UBR resemble structurally and are separated mutually by a steep (strike-slip) fault. The fault separates the LBR and UBR from the QN. Interaction of different factors: change in overburden pressure, rate of deformation and uplift in the different parts of the subsurface anticlines moved and accumulated Gachsaran Formationtowards both limbs of the anticlines.https://dergipark.org.tr/tr/download/article-file/3337944subsurface oil fieldscentral zagrosiranlower and upper balarud anticlines
spellingShingle Ahmad Radmehr
Soumyajit Mukherjee
Mohammad Seraj
Raana Razavi Pash
Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
Bulletin of the Mineral Research and Exploration
subsurface oil fields
central zagros
iran
lower and upper balarud anticlines
title Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
title_full Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
title_fullStr Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
title_full_unstemmed Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
title_short Structural relationship between subsurface oil fields in the North Dezful Embayment: Qaleh Nar, Lower and Upper Balarud Anticlines (central Zagros, Iran)
title_sort structural relationship between subsurface oil fields in the north dezful embayment qaleh nar lower and upper balarud anticlines central zagros iran
topic subsurface oil fields
central zagros
iran
lower and upper balarud anticlines
url https://dergipark.org.tr/tr/download/article-file/3337944
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