Induced and Ambient Crustal Seismicity under the Ghawar Oil-Gas Fields, Saudi Arabia

摘要

The Ghawar anticline (GA) is the super-giant anticline belonging to a set of giant anticlines called the Rayn anticlines (RA) developed in the Eastern Province (EP), Saudi Arabia. The RA is situated within the Arabian block microplate forming the distant foreland of the Zagros. For the first time, using the ‘Reviewed ISC Earthquake Catalogue’ for the period of 1970-2010, it is demonstrated that the EP crust is seismogenic down to a depth of ～15 km or more and has a typical surface width of ～220 km; this width is ostensibly six-times wider than that of GA. The Saudi Geological Survey (SGS) Earthquake Network Catalogue is utilized to study local seismicity. The GA is locally seismically active such that 826 events have occurred during the period of 2005-2010, with a maximum magnitude of ML 4.24. Magnitude completeness (Mc) analysis, based on the assumption of self-similarity, suggests that all local earthquakes above a cut-off magnitude of 32.7 have been detected in EP. Certain basic estimates on the average depth of origin of the induced events and histogram plot on the frequency of induced and ambient (natural) seismicity are illustrated. The induced events came almost in equal proportions from the Uthmaniyah-Hawaiyah and Haradh production divisions belonging to the central and southern oil/gas Fields in GA. Poroelastic parameters of the reservoir are reviewed with respect to the induced seismicity. Focal-depth distribution of events along the strike direction of seismic zones follows the ‘En-Nala axis’ in the GA and is used, together with ISC data, to broadly define the seismogenic crust from a 3D-perspective. Seismic activity below both production divisions is supposedly triggered by hydrocarbon fluid-extraction; locally triggered seismicity shows better correlation to mutually opposite reverse faults transgressing the Haradh and Uthmaniyah-Hawaiyah production divisions under the influence of regional compressive stress oriented along N40°E. Results from fo