Results 51 to 60 of about 1,036 (111)
T6SS-5 and the cGAS-STING pathway in Burkholderia pseudomallei infection and immunity
Burkholderia pseudomallei is a causative agent of melioidosis that can infect humans and animals in endemic countries, specifically in Southeast Asia and tropical Australia. A fundamental component for the pathogenesis of Burkholderia pseudomallei is the
Noreafifah Semail +6 more
doaj +1 more source
Klasik İslâm Tarihi Kaynaklarında Nübüvvet Mührü
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
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
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
SSZ Semail Ophiolite vs MORB Masirah Ophiolite: A Perspective from Podiform Chromitites
One of the major topics of debate in ophiolite geology is the original tectonic setting of ophiolites. New studies show that most ophiolites are formed more frequently in a supra‐subduction zone (SSZ) environment and that only a very small number of ...
S. Nasir
semanticscholar +1 more source
Abstract The Fujairah basin in the Gulf of Oman experienced a complex tectonic evolution related to Late Cretaceous ophiolite obduction and Oligocene‐Miocene Zagros continental collision. The structure of the foreland basin in Oman‐UAE is well‐known, but the structure and evolution of the hinterland basin behind the obducted ophiolite and underlying ...
M. Y. Ali +5 more
wiley +1 more source
The basal mantle of the Semail ophiolite directly overlying the metamorphic sole has been affected by a late and relatively low temperature ductile deformation event, ascribed to the deformation of the mantle just above the plate interface during ...
C. Prigent +4 more
semanticscholar +1 more source
Mantle Potential Temperature Estimates of Basalt from the East Taiwan Ophiolite
The East Taiwan Ophiolite (ETO) is a fragment of the eastern-most South China Sea that was accreted to the Eurasian margin during the Pliocene and is a member of the Western Pacific and Cordilleran belt ophiolite group.
J. Gregory Shellnutt Robert B.-J. Hsieh
doaj +1 more source
Several samples of laterites were collected from four paleosol profiles, Ibra, East Ibra, Al-Russayl, and Tiwi representing the vertical lithological variation within each profile.
Salah Al Khirbash, Khadija Semhi
doaj +1 more source
Abstract Serpentinization, a consequence of water‐rock interaction in mafic and ultramafic rocks, refers to the hydrothermal alteration of olivine and pyroxene with serpentine as the typical product. Magnetite is produced in variable amounts during this serpentinization process. Here, we conducted a systematic rock magnetic study on the serpentinite of
Yuzhen Zhang +5 more
wiley +1 more source

