Tectonic evolution of the Palmyra zone, Syria
Conference
·
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:5720554
- Amoco production Co., Houston, TX (USA)
The Palmyra foldbelt extends approximately 350 km northeast from its intersection with the Dead Sea transform near Damascus. The surface expression of this feature is a southeast-verging fold-and-thrust belt that brings rocks as old as Triassic to the surface in fault contact with Upper Cretaceous and Tertiary rocks. The palmyra region is first recognized as a subsiding trough from at least Triassic and possibly Permian time through middle Tertiary. This subsidence increases south-westward, reaching a reported maximum of 6 km of sediment north of Damascus, and is related to right-lateral motion along the eastern margin of the opening southern branch of the Neotethys sea as the Cimmerian continent moved northward away from northeast AFrica during Permian-Triassic time. Extension and subsidence continued through the Jurassic and Cretaceous, interrupted by uplift and erosion from Late Jurassic to Early Cretaceous in the northeastern part of the zone. Compression and inversion of the Palmyra zone begin during Miocene time with the initiation of left-lateral displacement on the Dead Sea transform system related to the continued opening of the Red Sea and the failure of the Gulf of Suez rift system. Approximately 105 km of offset are reported for the Dead Sea transform along the Jordan-Israel border segment, while 60 km are reported in Syria north of Lebanon. The Palmyra foldbelt accommodates this discrepancy through oblique shortening, possibly utilizing pre-existing extensional fault systems.
- OSTI ID:
- 5720554
- Report Number(s):
- CONF-8809346--
- Conference Information:
- Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Journal Volume: 72:8
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
ASIA
CENOZOIC ERA
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC HISTORY
GEOLOGIC STRUCTURES
JURASSIC PERIOD
MESOZOIC ERA
MIDDLE EAST
PALEOZOIC ERA
PERMIAN PERIOD
RIFT ZONES
SYRIA
TECTONICS
TERTIARY PERIOD
TRIASSIC PERIOD
020200* -- Petroleum-- Reserves
Geology
& Exploration
ASIA
CENOZOIC ERA
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
GEOLOGIC AGES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC HISTORY
GEOLOGIC STRUCTURES
JURASSIC PERIOD
MESOZOIC ERA
MIDDLE EAST
PALEOZOIC ERA
PERMIAN PERIOD
RIFT ZONES
SYRIA
TECTONICS
TERTIARY PERIOD
TRIASSIC PERIOD