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- W2185603421 abstract "Layering is well pronounced in several exposures of gab- broid rocks within certain zones, subzones and horizons of the Semail ophiolite (Late-Cretaceous). From Khor Kalba Horizon - Wadi Hatta Zone, southward to Khor Fakkan Zone, and northward passing through Bathnah Zone (Al-Fujairah - Masafi road), most layered gab- bros appear to have formed with their steeply inclined to ver- tical; horizontal is rarely observed. It is probably formed in situ on cooling walls or plated onto the walls by density or convection currents (current deposition). This mechanism, may however, not be responsible for the formation of all types of found in the present work. Preferred orientations of magmatic flow structure layering are compatible to a large extent with the major structural trends identified in the United Arab Emirates. The NW orientation (Hatta Zone-Wadi Ham trend), the NE orientation (Dibba Zone trend) and NS orienta- tion (overthrusted Semail ophiolite nappe) are consistent with the ma- jor tectonic trends identified in the UAE. This may lead to a better un- derstanding of the orientation of that has been controlled by the regional tectonism and may be the dynamics of magma chambers at oceanic spreading center." @default.
- W2185603421 created "2016-06-24" @default.
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- W2185603421 date "1999-01-01" @default.
- W2185603421 modified "2023-09-27" @default.
- W2185603421 title "Layering in Gabbroid Rocks from Semail Ophiolite, United Arab Emirates: Characterization, Tectonic Control on Origin and Orientation" @default.
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