Book Chapter
6: Kinematic, Thermal, and Petroleum Modeling of the Northern Emirates
Author(s)
Jean-Paul Callot
;
Jean-Paul Callot
IFPEN, Geosciences Division, 1-4 Avenue de Bois-Préau, Rueil-Malmaison 92852, France (e-mail: jean-paul.callot@univ-pau.fr; Francois.roure@ifpen.fr; J-luc.faure@beicipfranlab.fr);
1
Present address: E2S-Univ. Pau & Pays Adour, TOTAL-CNRS LFCR-IPRA, Pau France; 2
Also at Tectonic Group, Utrecht University, Utrecht, the Netherlands (mail of F. Roure: francoisroure84@gmail.com); 3
Present address: BEICIP-Franlab, Avenue Napoléon Bonaparte, 92852 Rueil-Malmaison, France
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François Roure
;
François Roure
IFPEN, Geosciences Division, 1-4 Avenue de Bois-Préau, Rueil-Malmaison 92852, France (e-mail: jean-paul.callot@univ-pau.fr; Francois.roure@ifpen.fr; J-luc.faure@beicipfranlab.fr);
1
Present address: E2S-Univ. Pau & Pays Adour, TOTAL-CNRS LFCR-IPRA, Pau France; 2
Also at Tectonic Group, Utrecht University, Utrecht, the Netherlands (mail of F. Roure: francoisroure84@gmail.com); 3
Present address: BEICIP-Franlab, Avenue Napoléon Bonaparte, 92852 Rueil-Malmaison, France
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Jean-Luc Faure
;
Jean-Luc Faure
IFPEN, Geosciences Division, 1-4 Avenue de Bois-Préau, Rueil-Malmaison 92852, France (e-mail: jean-paul.callot@univ-pau.fr; Francois.roure@ifpen.fr; J-luc.faure@beicipfranlab.fr);
1
Present address: E2S-Univ. Pau & Pays Adour, TOTAL-CNRS LFCR-IPRA, Pau France; 2
Also at Tectonic Group, Utrecht University, Utrecht, the Netherlands (mail of F. Roure: francoisroure84@gmail.com); 3
Present address: BEICIP-Franlab, Avenue Napoléon Bonaparte, 92852 Rueil-Malmaison, France
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Mihai Tarapoanca
Mihai Tarapoanca
Danubian Energy Consulting,35-37 Academiei street, entrance A, 6th floor, 11th suite, Bucharest 1, Romania (e-mail: mtarapoanca@danubianenergy.com);
4
Present address: Danubian Energy Consulting, Bucharest, Romania
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Published:January 01, 2018
ABSTRACT
Deep seismic profiles, recorded in the foothills of the Northern Emirates, image the thrust-belt architecture and document the wide underthrusting of Mesozoic sedimentary units in the footwall of the Hawasina–Sumeini allochthon in the Dibba Zone, beneath the Semail Ophiolite. Integrated structural and geophysical modeling helped to constrain the structural architecture of two regional transects crossing the foreland and adjacent foothills. 2-D forward kinematic and thermal modeling was performed with Thrustpack® along the transects, whereas CERES2D® complete petroleum system modeling was subsequently performed along the northern transect. One hundred twenty kilometers (75 mi) of convergence occurred from the Santonian to...
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figures&tables
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contents
Contents
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references
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related
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Contents
AAPG Memoir
Petroleum Systems Analysis—Case Studies
Author(s)
The American Association of Petroleum Geologists
Volume
114
Copyright:
© 2017 The Geological Society of America. All rights reserved.
ISBN electronic:
9781629812786
Publication date:
January 01, 2018
GeoRef
Index Terms/Descriptors
- Arabian Peninsula
- Asia
- burial
- calibration
- fission-track dating
- fluid flow
- fluid inclusions
- geochronology
- geophysical methods
- geophysical profiles
- geophysical surveys
- hydrothermal alteration
- inclusions
- kinematics
- maturity
- metasomatism
- migration
- Oman
- paleotemperature
- permeability
- petroleum
- petroleum exploration
- pore pressure
- porosity
- reservoir rocks
- saturation
- sealing
- seismic methods
- seismic profiles
- Semail Ophiolite
- source rocks
- spatial distribution
- structural controls
- surveys
- tectonics
- tectonostratigraphic units
- thermal maturity
- thermal properties
- two-dimensional models
- United Arab Emirates
- petroleum systems
- CERES2D
- Hawasina-Sumeini Allochthon
Latitude & Longitude
References
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