Abstract
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 four composite focal mechanism solutions also support this contention.
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References
Afifi, A.M. (2004) Ghawar: The anatomy of the world’s largest oil field. Saudi Aramco.www.searchanddiscovery.com/documents
Aki, K. (1965) Maximum likelihood estimate of b in the formula log N =a–bM and its confidence limits. Bull. Earthquake Res. Inst., Univ Tokyo, v.43, pp.237–239
Al-Amri, A.M. and Rodgers, A.J. (2013) Improvement of seismicity parameters in the Arabian Shield and Platform using earthquake location and magnitude calibration. In: K. Al Hosani et al. (Eds.), Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues, Frontiers in Earth Sciences, Springer-Verlag Heidelberg, Chapter 14.
Al-Shamrani, A.B.S. (2007) Micro-Seismicity of Al-Ghawar Oil Field Eastern Saudi Arabia. Master’s Thesis, Dept. Geology, King Saud University, Riyadh, Saudi Arabia.
Bartholomew, M.J., Stickney, M.C., Wilde, E.M. and Dundas, R.G. (2002) Late Quaternary paleoseismites: Syndepositional features and section restoration used to indicate paleoseismicity and stress-field orientations during faulting along the main Lima Reservoir Fault, southwestern Montana. In: F.R. Ettensohn, N. Rast, C.E. Brett, (Eds.), Ancient Seismites. Geol. Soc. Amer., Special Paper, no.359, pp.29–47.
Bonnet, A.D. (2015) Oilfield performance–Ghawar Oilfield (Saudi Arabia). GeoVille, www.geoville.com
Bou-Rabee, F. and Mukhopadhyay, M. (2008) Oilfield seismicity in Kuwait and its environmental impact. In: Near-surface Geophysics and Human Activity. Proc. 3rd Internat. Conf. Environ. Engg. Geophys., June 2008, Wuhan, China, Science Press, U.S.A.
Chang, K.W. and Segall, P. (2016) Injection-induced seismicity on basement faults including poroelastic stressing. Jour. Geophys. Res., Solid Earth, v.121, doi:10.1002/2015JB012561.
Dahm, T., Hainzl, S., Becker, D. and the FKPE Group DINSeis. (2013) How to discriminate induced, triggered and natural seismicity.European Center for Geodynamics & Seismology, Luxembourg, Proc. Workshop Induced Seismicity, v.30, Nov.15-17, 2010.
Davis, S.D. and Frohlich, C. (1993) Did (or will) fluid injection cause earthquakes? Criteria for a rational assessment. Seism. Res. Lett., v.64, pp.207–224.
de Waal, J.A., Muntendam-Bos, A.G. and Roest, J.P.A. (2015) Production induced subsidence and seismicity in the Groningen gas field–can it be managed? Proc. IAHS, v.372, pp.129–139. doi:10.5194/piahs-372-129-2015
Edgell, H.S. (1992) Basement tectonics of Saudi Arabia as related to oilfield structures. In: Richards, M., et al. (Eds.), Basement Tectonics, Kluwer Acad. Publishers, pp.169–193.
Elawadi, E. and Mukhopadhyay, M. (2017) Subsurface configuration of the Rayn Anticlines and evidences for plate margin kinematics in the East Arabian Block, Saudi Arabia–Reinterpreted results from potential field data. (submitted)
Endo, E., Zahran, H., Nofal, H. and Hadidy, S. (2007) The Saudi National Seismic Network. Seismo. Res. Lett., v.78(4), pp.439–445.
Foulger, G.R., Wilson, M., Gluyas, J., Julian, B.R. and Davies, R. (2015) A global review of human-induced earthquakes. Community.dur.ac.uk/g.r.foulger/FTP/Human Induced Earthquakes_Durham.pdf, pp. 292.
GEOEXPRO (2010) The application of microseismics in the Oil and Gas Industry. Ghawar, Saudi Arabia: The King of Giant Fields. GeoExpro.com, v.7(4), pp.58–63.
Gibson, G. and Sandiford, M. (2013) Seismicity and induced earthquakes. Background paper to NSW Chief Scientist and Engineer (OCSE). Univ. Melbourne, pp.33.
Greg Croft Inc.(1996) TheGhawar Oil Field, Saudi Arabia. http://www.gregcroft.com/ghawar.ivnu
Guglielmi, Y., Cappa, F., Avouac, J-P., Henry, P. and Elsworth, D. (2015) Seismicity triggered by fluid injection–induced aseismic slip. Science, v.348(6240), pp.1224–1226.
Ingebritsen, S.E. and Manning, C.E. (2010) Permeability of the continental crust: dynamic variations inferred from seismicity and metamorphism. Geofluids, v.10, pp.193–205.
International Seismological Centre, On-line Bulletin, http://www.isc.ac.uk, Internat. Seis. Centre, Thatcham, United Kingdom. (2010)
Konert, G., Afifi, A.M., Al-Hazri, S.A. and Droste, H.J. (2001) Paleozoic stratigraphy and hydrocarbon habitat of the Arabian Plate. GeoArabia, v.6(3), pp.407–442.
Langenbruch, C. and Zoback, M.D. (2016) How will induced seismicity in Oklahoma respond to decreased saltwater injection rates? Science Advances, 2: e1601542, pp. 1–9.
Lucia, F.J., Jennings, J.W. and Rahnis, M. (2002) Permeability and rock fabric from wireline logs, Arab-D reservoir, Ghawar Field, Saudi Arabia. GeoArabia, v.6(4), pp.619–646.
Maxwell, S. (2013) Unintentional seismicity induced by hydraulic fracturing. FOCUS Article, Schlumberger, CSEG Recorder, pp.40–49.
Mignan, A. and Woessner, J. (2012) Estimating the magnitude of completeness in earthquake catalogs. Community Online Resource for Statistical Seismicity Analysis. doi:10.5078/corssa-00180805.
Mogren, S. and Mukhopadhyay, M. (2013) Study of seismogenic crust in the Eastern Province of Saudi Arabia and its relation to the seismicity of the Ghawar Fields. Abstract, Am. Geophys. Union, Fall Meeting, 9-13 Dec.
Muntendam-Bos, A. G. and de Waal, J.A. (2013) Reassessment of the probability of higher magnitude earthquakes in the Groningen gas field: SodM technical report, http://www. sodm.nl/sites/default/files/redactie/rapport%20analyse%20 aardbevingsgegevens%20 groningse% 20gasveld %2016012013
National Research Council, (2013) Induced Seismicity Potential in Energy Technologies, Washington, D.C.: The National Academies Press. doi:10.17226/13355, pp.262.
Petersen, M.D., Mueller, C.S., Moschetti, M.P., Hoover, S.M., Llenos, A.L., Ellsworth, W.L., Michael, A.J., Rubenstein, J.L., McGarr, A.F. and Rukstales, K.S. (2016) Seismic-hazard forecast for 2016 including induced and natural earthquakes in the Central and Eastern United States. Seism. Res. Lett., v.87(6), pp.1327–1341. Doi:10.1785/0220160072
Sagar, S. and Leonard, M. (2008) Mapping the magnitude of completeness of the Australian earthquake catalogue. Publn. Geoscience Australia, pp.8.
Sahin, A., Ali, A.Z., Saner, S. and Menouar, H. (2007) Permeability anisotropy distributions in an Upper Jurassic carbonate reservoir, Eastern Saudi Arabia. Jour. Pet. Geol., v.30(2), pp.147–158.
Saner, S. and Sahin, A. (1999) Lithological and zonal porosity-permeability distributions in the Arab-D reservoir, Uthmaniyah Field, Saudi Arabia. AAPG Bull., v.83(2), pp.230–243.
Saner, S., Al-Hinai, K. and Perincek, D. (2005) Surface expression of the Ghawarstructure, Saudi Arabia. Marine Pet. Geol., v.22, pp.657–670.
Saudi Geological Survey Jeddah. National Centre for Earthquakes and Volcanoes. www.sgs.org.sa
Švancara, J., Havir, J. and Conrad, W. (2008) Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity. Stud. Geophys. Geod., v.52, pp.567–588.
Segall, P. and Fitzgerald, S.D. (1998) A note on induced stress changes in hydrocarbon and geothermal reservoirs. Tectonophys., v.289, pp.117–128.
Segall, P. and Lu, S. (2015) Injection-induced seismicity: Poroelastic and earthquake nucleation effects. Jour. Geophys. Res., Solid Earth, v.120: 5082–5103. doi:10.1002/2015/B012060
Sibson, R.H. (1982) Fault zone models, heat flow and the depth distribution of earthquakes in the continental crust of the United States. Bull. Seismol. Soc. Amer., v.72(1), pp.151–163.
Smit, L., Fagerenga, A., Braeuer, B. and Stankiewicz, J. (2015) Microseismic activity and basement controls on an active intraplate strike-slip fault, Ceres-Tulbagh, South Africa. Bull. Seismol. Soc. Amer., v.105, pp.1540–1547.
Sorkhabi, R. (2010) The King of Giant Fields. GEO Expro, v.4(7). http://www.geoexpro.com
Steineke, M., Harriss, T.F., Parsons, K.R. and Berg, E.L. (1979) Geologic map of the Western Arabian Gulf Quadrangle, Kingdom of Saudi Arabia. Geologic Map GM-208 A. Min. Pet. Min. Res., Dir. Gen. Min. Res., Jeddah, Saudi Arabia.
Suckale, J. (2009) Induced seismicity in hydrocarbon fields. Advances in Geophysics, v.51, Chapter 2, pp.1–52.
Talwani, P. (2000) Seismogenic properties of the crust inferred from recent studies of reservoir induced seismicity–Application to Koyna. Curr. Sci., v.79(9), pp.1327–1333.
Talwani, P. and Acree, S. (1984) Pore pressure diffusion and the mechanism of reservoir induced seismicity. PAGEOPH, v.122.
van Thienen-Visser, K. and Breunese, J.N. (2015) Induced seismicity of the Groningen gas field: History and recent developments. The Leading Edge, Special Section: Injection-induced Seismicity, June 2015, pp.664–671.
Weijarmars, R. (1998) Plio-Quaternary movement of the East Arabian Block. GeoArabia, v.3(4), pp.509–540.
Wender, L.E., Bryant, J.W., Dickens, M.F., Neville, A.S. and Al-Moqbel, A.M. (1998) Paleozoic (pre-Khuff) hydrocarbon geology of the Ghawar area, eastern Saudi Arabia. GeoArabia, v.3, pp.273–302.
Wiemer, S. and Wyss, M. (2000) Minimum magnitude of completeness in earthquake catalogs: examples from Alaska, the Western United States, and Japan. Bull. Seismol. Soc. Amer., v.90, pp.859–869.
Zahran, H.M., El hadidy, S. and Yosef, K. (2010) Recent earthquake activity at Haradh region, Western Saudi Arabia. European Center for Geodynamics & Seismology, Luxembourg, Proc. Workshop Induced Seismicity, v.30, Nov. 15-17, 2010.
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Mukhopadhyay, M., Elawadi, E., Mukhopadhyay, B. et al. Induced and Ambient Crustal Seismicity under the Ghawar Oil-Gas Fields, Saudi Arabia. J Geol Soc India 91, 449–456 (2018). https://doi.org/10.1007/s12594-018-0878-x
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DOI: https://doi.org/10.1007/s12594-018-0878-x