Titlebook: Lithosphere Dynamics and Sedimentary Basins of the Arabian Plate and Surrounding Areas; François Roure,Ammar A. Amin,Mansour A. M. Al Garn

摘要记录

François Roure,Ammar A. Amin,Sami Khomsi,Mansour A. M. Al Garni

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Crustal and Upper Mantle Structures Beneath the Arabian Shield and Red Seaor Rayleigh and 20 to 70 s for Love waves) and teleseismic receiver functions for lithospheric velocity structure. The method relies on an initial grid search for a simple crustal structure, followed by a formal iterative inversion, an additional grid search for shear wave velocity in the mantle and

Provenance

Pressure and Thermal Regimes and Systems in the Sedimentary Sequence of Central and Eastern Saudi Arre systems by stratigraphic seals, but these are locally breached by unconformities or faults forming local anomalies. Geothermal gradients illustrate shallow and deep thermal regimes (STR and DTR) separated by a high thermal conductivity zone (HTCZ). The STR extends from land surface to 8000 ft, wi

宴会

Organonitrile

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Styles of Salt Tectonics in the Sab’atayn Basin, Onshore Yemenf the diapiric walls in the basin are controlled by large normal faults on their updip flanks. As the post-Cretaceous sedimentary cover is largely missing in the study area, the assumed reactivation of salt structures during the Cenozoic remains poorly constrained. The interpreted changes in the sty

一起

The Effect of the Palmyra Trough and Mesozoic Structures on the Levant Margin and on the Evolution ohe pre-existing structures on the growth of the restraining bend. Consequently, the pre-existing structures, which are believed to be part of the Palmyra basin structural system, attest that the latter extends westward to the Levant margin forming its westward termination. The evolution and propagat

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