Titlebook: Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues; Khalid Al Hosani,Francois Roure,Stephen Lokier Conference pr

Grating

Haphazard

Paleo-Fluids Characterisation and Fluid Flow Modelling Along a Regional Transect in Northern United clastic units of the Hawasina–Sumeini allochthon, which derive from the former paleo-slope domain and a more distal basinal portion of the Arabian margin of the Tethys, respectively. All these tectonic units display numerous evidences of paleo-fluid circulations, accounting for dolomitisation and re

广大

Diagenesis of the Khuff Formation (Permian–Triassic), Northern United Arab EmiratesLower Triassic carbonate rocks, which are equivalent to the Khuff Formation. The studied succession,which outcrops in the Ras Al Khaimah region, northern United Arab Emirates, comprises three formations, including the Bih, the Hagil, and the Ghail formations. The study focuses on unraveling the cond

Incumbent

Evidence for Mantle Exhumation Along the Arabian Margin in the Zagros (Kermanshah Area, Iran) exposed in this area were formerly interpreted as originated fromTethys ocean and other residual Tethys oceanic domains all situated northeast of the Bisotoun platform. However, the structural relationships between these ultramafic units remained unclear. New field work in the Kermanshah–Harsin are

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CRACY

Preliminary fault analysis and paleostress evolution in the Makran Fold-and-Thrust Belt in Iran. Field observation documents the importance of E-W thrust faulting associated with E-W buckle folding, which is consistent with the main shortening direction expected in the study area, the convergence zone between the Arabian and Eurasian plates. Two main paleostress tensor directions are distingu

Magisterial

Improvement of seismicity parameters in the Arabian Shield and Platform using earthquake location anticularly, Arabian Shield and Arabian Platform are aseismic, the area is ringed with regional seismic sources in the tectonically active areas of Iran and Turkey to the northeast, the Red Sea Rift bordering the Shield to the southwest, and the Dead Sea Transform fault zone to the north. Therefore, t

VOC

Seismotectonics and seismogenic source zones of the Arabian Platformng in Arabian Gulf cities. The Arabian Gulf is underlain by deep sedimentary structure, nearly 10 km deep, and is adjacent to one of the most seismically active intra-continental fold-and-thrust belts on Earth, the Zagros Mountains. Broadband records in the western shore of the Gulf from earthquakes

Vasoconstrictor

Seismic zones regionalization and hazard assessment of SW Arabian Shield and Southern Red Sea Region°–19°N and Longitudes 39°–45°E in the period of 200–2005 A.D. with magnitudes ranges from 2 ≤ M ≤ 8.0. The area of interest has a complicated geological structures and tectonics. The epicentral distribution of both historical and instrumental earthquakes shows a general correlation with the regional

不如屎壳郎

Structural and Stratigraphic Evolution of Abu Dhabi in the Context of Arabiatemperate climate conditions ensured that formuch of its early existence, Arabia was the site of mainly quartz-rich deposits. Later in the Neoproterozoic, however, extensive stromatolitic carbonate deposition took the lead, culminating around the Cambro- Precambrian boundary with deposition of the e