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Title: Seismic reflection structure of intracratonic palmyride fold-thrust belt and surrounding Arabian platform, Syria

Journal Article · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:6934932
; ;  [1]; ; ; ;  [2]
  1. Cornell Univ., Ithaca, NY (USA)
  2. Syrian Petroleum Co., Damascus (Syria)

Seismic reflection and drill-hole data from central Syria provide a detailed view of the subsurface structure (10-15 km depth) of the relatively little-studied intracratonic Palmyride fold and thrust belt. The data set, together with surface geologic mapping, constrains a structural/stratigraphic section spanning the northeast sector of the belt and the surrounding subprovinces of the Arabian platform. The seismic reflection and drill-hole data show Mesozoic stratigraphic sequences thickening abruptly into the Palmyrides from the adjacent, arched Paleozoic platforms Neogene (alpine) folding and thrusting of the Mesozoic basin, as documented on the seismic data, are sharply restricted to the narrow width of the belt ({approximately}100 km), in contrast to the relatively undeformed Phanerozoic strata of the platforms to the north and south. The seismic and drill-hole data support the hypothesis that the palmyrides began as a Permian-Triassic failed rift connected to the Levantine passive continental margin, which was inverted and complexly deformed by the interfering effects of Cenozoic movements along the Dead Sea transform fault system and the Turkish Bitlis convergent zone. The seismic data provide a first view into the extent and depth of the early basin formation and subsequent compressional deformation, and as such represent a necessary element for constraining reconstructions of northern Middle East plate motions. 20 figs.

OSTI ID:
6934932
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (USA), Vol. 74:3; ISSN 0149-1423
Country of Publication:
United States
Language:
English

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