Changes

The geology of the Arabian plate, North Africa and parts of Southern Eurasia are often discussed independent of one another. Our approach has been to step back and look at the region from a plate-scale geologic perspective. The present day Arabian and North Africa plates evolved together as a single unit from the Precambrian. They were physically connected as they moved around the globe from the southern polar regions to their present day position in the northern hemisphere, sub-tropical belt. Throughout the Phanerozoic, these plates have been on the margin of a series of Tethys seaways, including the Proto-Tethys, Paleo-Tethys, and Neo-Tethys. The common evolution of these plates along the Tethys Margin led to many similarities in the regional geology, including similar paleogeographic, tectonic, stratigraphic and depositional settings which, in turn, led to the development of similar petroleum systems. Though there are numerous similarities across the margin, variations occur too, and these can be compared in the chapters that follow. One primary difference across the region was the transition from uniform platform sedimentation which occurred across North Africa and Arabia, to intracontinental sub-basins and rift-basins (Arabian plate and North Africa, respectively) in the Permian, which led to “pots” of source rock across the Tethyan Margin.

The geology of the Arabian plate, North Africa and parts of Southern Eurasia are often discussed independent of one another. Our approach has been to step back and look at the region from a plate-scale geologic perspective. The present day Arabian and North Africa plates evolved together as a single unit from the Precambrian. They were physically connected as they moved around the globe from the southern polar regions to their present day position in the northern hemisphere, sub-tropical belt. Throughout the Phanerozoic, these plates have been on the margin of a series of Tethys seaways, including the Proto-Tethys, Paleo-Tethys, and Neo-Tethys. The common evolution of these plates along the Tethys Margin led to many similarities in the regional geology, including similar paleogeographic, tectonic, stratigraphic and depositional settings which, in turn, led to the development of similar petroleum systems. Though there are numerous similarities across the margin, variations occur too, and these can be compared in the chapters that follow. One primary difference across the region was the transition from uniform platform sedimentation which occurred across North Africa and Arabia, to intracontinental sub-basins and rift-basins (Arabian plate and North Africa, respectively) in the Permian, which led to “pots” of source rock across the Tethyan Margin.

[[file:M106IntroFig01.jpg|thumb|300px|Basins, fields, and structures data from IHS International Energy Database (January 2010). Base map is ETOPO1 (Amante and Eakins<ref name=Amanteandeakins_2009>Amante, C., and B. W. Eakins, ETOPO1 1 Arc-minute global relief model: Procedures, data sources and analysis: NOAA Technical Memorandum NESDIS NGDC-24, 10 p., March 2009. http://ngdc.noaa.gov/mgg/global/global.html.</ref>]]

[[file:M106IntroFig01.jpg|thumb|300px|Basins, fields, and structures data from IHS International Energy Database (January 2010). Base map is ETOPO1 (Amante and Eakins<ref name=Amanteandeakins_2009>Amante, C., and B. W. Eakins, ETOPO1 1 Arc-minute global relief model: Procedures, data sources and analysis: NOAA Technical Memorandum NESDIS NGDC-24, 10 p., March 2009. http://ngdc.noaa.gov/mgg/global/global.html.</ref>).]]

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