Results 51 to 60 of about 181 (118)

The captives of Badr and their attitude and behavior after the Battle of Badr [PDF]

open access: yes, 2023
Yüksek Lisans TeziBedir Savaşı, Müslümanların Hicaz bölgesinde bir güç olarak tanınmasını sağlarken Mekke'deki Kureyş kabilesinin itibarını sarsmıştır. Güç dengelerinin değişiminde bu savaş büyük rol oynamış ve âdeta kırılma noktası olmuştur.
Güzeş, Raziye Gül
core   +1 more source

Detrital Zircon U–Pb Geochronology of the Muti Formation: Implications for Provenance and Evolution of the Oman Foreland Basin

open access: yesGeosciences
Detrital zircon U–Pb dating from the Muti Formation sheds light on sediment sources and foreland basin development along the northeastern Arabian margin during the Late Cretaceous.
Iftikhar Ahmed Abbasi   +5 more
doaj   +1 more source

Uplift Dynamics of the Obducted Northeastern Continental Margin of the Arabian Peninsula, Sultanate of Oman

open access: yesGeochemistry, Geophysics, Geosystems, 2023
Eustatic sea level changes and vertical tectonic movements are producing uplifted paleoshorelines. Along subduction zones, uplifted terraces are used to study fault activities and, overall, allow to interpret the tectonic history of plate convergence ...
Kosmas Pavlopoulos   +7 more
doaj   +1 more source

Klasik İslâm Tarihi Kaynaklarında Nübüvvet Mührü

open access: yesAtebe, 2021
Nübüvvet mührü; (hâtemü’n-nübüvve) siyer, şemâil, hasâis, delâil türü İslâm Tarihi kaynaklarında yer almış, kimilerince Peygamberimizin nübüvvetinin tasdikinde delil sayılmıştır. Nübüvvet mührü bir alamet olarak Ehl-i kitap mensuplarının kaynaklarında da
Nejla Ceyhan
doaj   +1 more source

On the Subduction Polarity Beneath the Semail Ophiolite

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 7, July 2025.
Abstract 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 ophiolite and subsequent obduction remain debated.
Simone Pilia
wiley   +1 more source

Hakim Mehmed Efendi'nin Manzum Hilyesi

open access: yesCumhuriyet Üniversitesi İlahiyat Fakültesi Dergisi, 2007
Kaynaklara göre asıl adı Seyyid Mehmed olan Hakim'in doğum tarihi bilinmemektedir. H. 11841 M. 1770'te vefat eden Hakim Mehmed Efendi iyi bir eğitim görmüştür ve yirmi kadar eseri bulunmaktadır.
MEHTAP ERDOĞAN
doaj  

Mineralogical characterisation of aeolian sands using multispectral satellite datasets: Implications for dune field evolution, Wahiba Dune Field, Oman

open access: yesEarth Surface Processes and Landforms, Volume 50, Issue 6, May 2025.
This study develops a remote sensing methodology that integrates high‐resolution satellite imagery with field validation to map the Wahiba Dune Field of Oman. Findings reveal the sensitivity of contemporary geomorphic surfaces to local sediment dynamics and highlight the value of multi‐scale analysis in interpreting dune field evolution.
David Cousins   +7 more
wiley   +1 more source

Tectono-thermal evolution of Oman's Mesozoic passive continental margin under the obducting Semail Ophiolite: a case study of Jebel Akhdar, Oman [PDF]

open access: yesSolid Earth, 2019
We present a study of pressure and temperature evolution in the passive continental margin under the Oman Ophiolite using numerical basin models calibrated with thermal maturity data, fluid-inclusion thermometry, and low-temperature thermochronometry and
A. Grobe   +9 more
doaj   +1 more source

Quantitative Microstructural Analysis of Exhumed Epidote‐Amphibolites and Plate Interface Rheology in Warm Subduction Zones

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 4, April 2025.
Abstract Epidote‐amphibolites form along the plate interface during subduction infancy and are stable in warm, mature subduction zones that generate slow earthquakes. Epidote‐amphibolite rheology therefore likely influences plate‐scale processes during plate boundary formation and grain‐scale processes that give rise to slip transients.
Laurens H. Kleijbeuker   +3 more
wiley   +1 more source

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