Zagros Thrust Belt
The NW-SE-trending Zagros thrust belt extends for approximately 2000 km from the Taurus Mountains in Turkey and Syria in the northwest, through northeast Iraq (Kurdistan) and the central Iran Plateau, southeastward to the Persian Gulf foreland towards the southwest. This prominent thrust belt is a very prolific hydrocarbon province and hosts more than 5% of the world’s hydrocarbon reserves (Cooper, 2007). Intense exploration has been mainly focused on the productive Fars Zone and Dezful Embayement regions of Iran in the central sector of the Zagros thrust belt. During the last years, the northwestern sector of the Zagros, extending over the Kurdistan region of northeast Iraq and the Lorestan province of Iran has increasingly received attention related to a renewed interest for hydrocarbon exploration. According to the Oil & Gas Journal, Iran has an estimated 158 billion barrels of proved crude oil reserves, representing almost 10% of the world’s crude oil reserves. Whilst the geological reasons for much of this success are fairly simple to understand, predicting the best areas to target is somewhat more complex and requires a more regional geological understanding for assessing the hydrocarbon perspectivity.
Exploration success in the Kurdistan and Lorestan hydrocarbon provinces, as in many other parts of the Middle East, is charcterised by a fortuitous juxtaposition of source rock, reservoir and seal in structural traps. Common seepage in the region testifies a working petroleum system, principally driven by the thick, bituminous limestones of the Jurassic Sargelu and Naokelekan Formations.
Hydrocarbons are mostly trapped within broad four-way-dip closure thrust-related anticlines hosting important fractured carbonate reservoirs at various stratigraphic levels wihtin the Meso-Cenozoic sequence.
The understanding of the regional tectonic evolution, styles of compressional deformation and controls on regional stress patterns are helpful in unravelling the distribution fracture networks for characterising fractured reservoirs. The integration of remote sensisng analysis, seismic interpretation, well data and the orientation of the present-day stress field lead to build consistent structural models that can be used during exploration and development phases.
This study reviews the structural style over the Kurdistan region of northeast Iraq (Kirkuk Embayement) and the Lorestan province of Iran (Pusht-e Kun Arc) from regional to local-scale. The report includes an integrated analysis of various data and methodologies in order to contribute in a better understanding of the compressional deformation styles, mechanisms and evolution of the trap-forming structures. These latter factors are eventually discussed to evaluate their impact on hydrocarbon distribution. For this purpose, a series of regional cross-sections, constructed by integrating surface and available subsurface data, is presented through the main hydrocarbon fields and open license blocks. The report provides also an overview of the current exporation activities, fields and discoveries in the Kurdistan and Lorestan regions, focusing on the play types and the existing exploration potentials in the area. Furthermore, the report is supplied with a GIS project where distribution maps (facies, plays, domains, paleogeographies etc.), wells database, culture and geo-referenced data are included.
ALBANIA, WESTERN GREECE & CRETE
HC POTENTIAL OF SHALLOW WATER MIOCENE CARBONATES IN THE MEDITERRANEAN SEA
POSSIBLE ANALOGUES OF THE EASTERN MEDITERRANEAN CRETACEOUS ISOLATED CARBONATE PLATFORMS
GEOLOGICAL FRAMEWORK AND IMPLICATION FOR THE HC PROSPECTIVITY IN THE WESTERN MEDITERRANEAN SEA
WESTERN IBERIAN ATLANTIC MARGIN
RIONI AND KURA BASINS PETROLEUM PROSPECTIVITY (GEORGIA AND AZERBAIJAN)