Results 191 to 200 of about 71,897 (268)
This work demonstrates that site‐selective sulfur doping effectively narrows the bandgap of polar 2D Ga2O3 monolayer while preserving the built‐in electric field, enabling efficient carrier separation and enhanced visible‐light absorption for photocatalytic water splitting.
Qi Li +10 more
wiley +1 more source
Trace element systematics constrain the origin of fluids that form gem-quality diamonds. [PDF]
Rakipov A +8 more
europepmc +1 more source
Coupled dissolution‐reprecipitation of early formed Cd‐, Fe‐, Ag‐ and Sb‐poor sphalerite through interaction with high‐temperature and high‐sulphur fugacity Cu‐rich fluids, responsible for the formation of the yellow ores, resulted in the formation of Cd‐, Fe‐, Ag‐ and Sb‐rich, heavily chalcopyrite‐diseased sphalerite and enrichment of critical metals ...
Manuel Nopeia +4 more
wiley +1 more source
Is the walk and trot efficiency a hereditary trait in primitive Konik Polski horses? [PDF]
Siemieniuch-Tartanus M +2 more
europepmc +1 more source
The composition of intrusive rocks suggests that the magma was likely generated in a subduction‐related setting. The arc crustal thickness in the Phnom Sro Ngam and Halo Prospects was probably < 40 km during emplacement. Zircon U–Pb age range indicates a correlation with Loei Fold Belt magmatic activity.
Sirisokha Seang +6 more
wiley +1 more source
On the potential origin of the zygote-like cancer stem cell with a focus on fusion for cell rescue. [PDF]
Cismaru CA +4 more
europepmc +1 more source
Early zircon saturation and crystallisation occur in mafic (52–54 wt.% SiO2) lavas at Tengchong volcanic field. These early formed zircons with high δ18O (6.6‰–7.9‰) indicates mantle enrichment by subducted supracrustal materials. ABSTRACT Late Pleistocene (< 0.2 Ma) mafic and evolved volcanic rocks occur in northern Tengchong Volcanic Field, SE ...
Lizhu Wang, Haibo Zou
wiley +1 more source
Architecting bioinspired nanocrystalline domains for ultimate robust and transparent cellulose photonic hydrogels. [PDF]
Li Q +7 more
europepmc +1 more source
The study outlines the tectono‐sedimentary evolution of the İnegöl Basin in north‐western Anatolia. Basin formation was controlled by interacting extensional and strike‐slip fault systems linked to uplift of the Uludağ Massif. Terrestrial sedimentation from the Miocene to Pleistocene is reconstructed using abundant fossil mammal assemblages that ...
M. Cihat Alçiçek +2 more
wiley +1 more source

