Brew, G. E., Litak, R. K., Seber, D., Barazangi, M., Sawaf, T., and Al-Imam, A.

Brew, G. E., Litak, R. K., Seber, D., Barazangi, M., Sawaf, T., and Al-Imam, A.

Basement depth and sedimentary velocity structure in the northern Arabian platform, Eastern Syria

Geophysical Journal International, 128, 617-631, 1997.

Abstract

Basement depth in the Arabian plate beneath eastern Syria is found to be much deeper than previously supposed. Deep-seated faulting in the Euphrates graben system is also documented. Data from a detailed, 300 km long, reversed refraction profile, with offsets up to 54 km, are analyzed and interpreted, yielding a velocity model for the upper ~ 9 km of continental crust. The interpretation integrates the refraction data with seismic reflection profiles, well logs and potential field data, such that the results are consistent with all available information. A model of sedimentary thicknesses and seismic velocities throughout the region is established. Basement depth on the north side of the Euphrates is interpreted to be around 6 km, whilst south of the Euphrates basement depth is at least 8.5 km. Consequently, the potentially hydrocarbon-rich pre-Mesozoic section is shown, in places, to be at least 7 km thick. The dramatic difference in basement depth on adjacent sides of the Euphrates graben system might suggest that the Euphrates is a suture zone, possibly inherited from Late Proterozoic accretion of the Arabian plate. Gravity modeling across the southeast Euphrates system tends to support this hypothesis. Incorporation of previous results allows us to speculate on the position of possible suture zones in Syria.

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Copyright Statement

Geophysical Journal International

Publisher: Blackwell Publishing on behalf of The Royal Astronomical Society and The Deutsche Geophysikalische Gesellschaft
Edited by: C.J. Ebinger (Managing Editor)
Print ISSN: 0956-540X
Online ISSN: 1365-246X

Key Figures and Captions

Figure 10: Map showing basement depths in Syria in kilometers below surface. Results from this study and previous refraction interpretation of Seber et al. (1993). Underlined data points are from selected deep well data. Shading represents locations of possible suture / shear zones.

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