Results 131 to 140 of about 1,077 (157)

Synchronous formation of the metamorphic sole and igneous crust of the Semail ophiolite: New constraints on the tectonic evolution during ophiolite formation from high-precision U–Pb zircon geochronology

, 2016
M. Rioux, J. Garber, A. Bauer, S. Bowring, M. Searle, P. Kelemen, B. Hacker   +6 more
semanticscholar   +1 more source

Recycled oceanic crust as a source for tonalite intrusions in the mantle section of the Khor Fakkan block, Semail ophiolite (UAE)

Geoscience Frontiers, 2019
Hosung Joun, S. Kokkalas, S. Tombros
semanticscholar   +1 more source

Düşünsel Mimarlık: Rönesans Ütopyaları Aracılığıyla Bir Örnekleme [PDF]

, 1978
Alsaç , Üstün
core  

Geochronological constraints on the metamorphic sole of the Semail ophiolite in the United Arab Emirates

, 2016
N. Roberts, R. Thomas, J. Jacobs
semanticscholar   +1 more source

On the Subduction Polarity Beneath the Semail Ophiolite

Journal of Geophysical Research: Solid Earth, Volume 130, Issue 7, July 2025.
The Semail ophiolite and the UAE‐Oman mountain range offer a rare window into continental subduction and exhumation. Despite almost half a century of conflicting studies, the geometry and number of subductions that characterized the formation of the ...
S. Pilia
semanticscholar   +2 more sources

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Extensional tectonics rooted in orogenic collapse: Long-lived disintegration of the Semail Ophiolite, Oman

, 2020
Significant post-orogenic extension of the renowned Semail Ophiolite and substrata in Oman resulted in the formation of metamorphic core complexes juxtaposed with an array of Maastrichtian-Paleogene extensional basins.
A. Braathen, P. Osmundsen
semanticscholar   +1 more source

Architecture of the crust and lithosphere beneath the Semail Ophiolite from ambient noise tomography and receiver functions: insights on the tectonic evolution of eastern Arabia

, 2021
The Semail Ophiolite is the world‘s largest and best exposed oceanic lithosphere on land and a primary reference site for studies of creation of oceanic lithosphere, initiation of subduction, geodynamic models of obduction, subduction and ...
C. Weidle, L. Wiesenberg, A. Scharf, P. Agard, A. El‐Sharkawy, F. Krüger, T. Meier   +6 more
semanticscholar   +1 more source

Postobductional Kinematic Evolution and Geomorphology of a Major Regional Structure—The Semail Gap Fault Zone (Oman Mountains)

Tectonics, 2019
The Semail Gap/Semail Gap Fault Zone is one of the most prominent tectonic features in the Oman Mountains and is located between the Jabal Akhdar Dome in the west and the Saih Hatat Dome to the east.
A. Scharf, F. Mattern, D. Moraetis, I. Callegari, C. Weidle   +4 more
semanticscholar   +1 more source

Moho topography and Flexural response of Semail ophiolite in the Southern Oman Mountains: New constraints from teleseismic receiver functions and gravity anomalies

Geophysical Journal International
The Semail Ophiolite in Oman represents one of the well-preserved ophiolite complexes globally and provides a unique window into the processes of obduction.
M. Ismaiel, Muhammed Rishal, Rajat Patel
semanticscholar   +1 more source

Evidence of postobductional, brittle and transtensional deformation: the lineamentary Issmaiya Fault Zone – insights from kinematic analyses and remote sensing data interpretation (Semail Ophiolite near Ibra, Oman Mts., Sultanante of Oman)

, 2020
The main Meso-Cenozoic tectonic event that affected northern Oman was the obduction of allochthonous Hawasina Basin-derived sedimentary and volcanic rocks as well as the Semail Ophiolite during the Late Cretaceous.
I. Callegari, A. Braathen, A. Scharf, F. Mattern, E. Holzbecher, Anfaal Al Kharosi, A. Al Hajri   +6 more
semanticscholar   +1 more source