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Seismic fabric and 3-D upper crustal structure of the southwestern intracontinental Palmyride fold belt, Syria

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dc.contributor.authorChaimov, T.
dc.contributor.authorBarazangi, M.
dc.contributor.authorAl-Saad, D.
dc.contributor.authorSawaf, T.
dc.contributor.authorKhaddour, M.
dc.date.accessioned2007-02-23T18:27:01Z
dc.date.available2007-02-23T18:27:01Z
dc.date.issued1993
dc.descriptionCopyright 1993, AAPG. Reprinted by permission of the AAPG whose permission is required for further use. See also: http://aapgbull.geoscienceworld.org/; http://atlas.geo.cornell.edu/syria/chaimov_aapg_bull_1993.htmlen_US
dc.description.abstractThe Palmyride fold belt, a 400 X 100 km transpressive belt in central Syria that is the northeastern arm of the Syrian Arc, which includes the Negev fold belt in the Sinai, is the result of Late Mesozoic and Cenozoic inversion of a Late Paleozoic and Mesozoic, NE-trending, linear intracontinental basin located within the northern Arabian platform. The southwestern Palmyrides, near the Dead Sea transform fault system and the Anti-Lebanon mountains, are characterized by short wavelength (5-10 km) en echelon folds separated by small intermontane basins that developed mainly in Neogene to Recent times. A new three-dimensional data cube, 60 X 70 km, generated on a Landmark Graphics (TM) workstation and based on approximately 700 km of two-dimensional seismic reflection profiles, elucidates the structure of the upper 10 km of the crust in the southwestern Palmyrides. Visualization of the subsurface structure, which is represented by a prominent Upper Cretaceous reflection surface in the data cube, is augmented by the topography and Bouguer gravity of the same region. Preexisting discontinuities, probable normal fault relicts of the Mesozoic Palmyride rift, likely controlled the development of individual Neogene thrusts. The new subsurface image shows important structural features not identified in outcrop. Short, WNW-trending transcurrent, or transfer, faults link the short, en echelon NE-trending thrust faults and blind thrusts of the Palmyrides. A pervasive regional decollement is not observed, even though Triassic evaporites host local detachments. There has been no wholesale transport of shallower strata on a regional decollement that decouples Mesozoic and Cenozoic rocks from underlying Paleozoic rocks. Unlike topographic relief, which only roughly resembles subsurface structures, the Bouguer gravity signature of the southwestern Palmyrides closely mimics underlying shallow geologic structures both on a large (~50 km wavelength) and a small (~5-10 km) scale. Relatively uncommon reflections from deformed Paleozoic rocks and the excellent correlation between Bouguer gravity and shallow structures indicate a general concordance between shallow Mesozoic and Cenozoic rocks and deeper Paleozoic rocks. Hence, Paleozoic rocks either deformed together with shallower strata, or structures within Paleozoic rocks controlled the development of shallower Neogene and younger structures. Our structural analysis and many other recent studies of the region are indicative of minor right-lateral shear coupled with compression in the Palmyrides.en_US
dc.format.extent34788 bytes
dc.format.mimetypeapplication/pdf
dc.identifier.citationAmerican Association of Petroleum Geologists Bulletin, vol. 77, p. 2032-2047, 1993en_US
dc.identifier.issn0149-1423
dc.identifier.urihttps://hdl.handle.net/1813/5400
dc.language.isoenen_US
dc.publisherAmerican Association of Petroleum Geologists (AAPG)en_US
dc.subjectSyriaen_US
dc.subjectPalmyride fold belten_US
dc.subjectSeismic reflectionen_US
dc.subjectBouguer gravityen_US
dc.titleSeismic fabric and 3-D upper crustal structure of the southwestern intracontinental Palmyride fold belt, Syriaen_US
dc.typeperiodicalen_US

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