Upconversion luminescence and temperature sensing characteristics of MgAl2O4 spinel doped with Er3+ and Yb3+ ions [PDF]
Nanorod-shaped MgAl2O4: xEr3+, 0.05Yb3+ (where x ranges from 0.003 to 0.015) were synthesized using a low-temperature hydrothermal method. This study investigates the microstructure, upconversion luminescence performance, and temperature sensing ...
Yang Lu +5 more
doaj +2 more sources
Pressure Dependence of Magnesite Creep [PDF]
We determined the activation volumes (V*) for polycrystalline magnesite with grain sizes of 2 and 80 µm deforming by low temperature plasticity (LTP) mechanisms (kinking and dislocation glide), diffusion creep, and dislocation creep at temperatures ...
Joseph W. Millard +9 more
doaj +3 more sources
The FTIR Spectra of Raw Magnesite and Sintered Magnesite [PDF]
Gopinath Damodaran, S. Gunasekaran
openalex +2 more sources
Removal of Silicon from Magnesite by Flotation: Influence of Particle Size and Mechanical Mechanism [PDF]
Ruinan Zhang, Zhaoyang Liu, Jingkun Yu
openalex +2 more sources
Deep carbon cycling during subduction revealed by coexisting diamond-methane-magnesite in peridotite [PDF]
Xiaoxia Wang +7 more
openalex +2 more sources
Research on the efficient flotation desilication of low-grade magnesite is of great significance for the sustainable development of magnesium resources.
Wenbao Liu +6 more
doaj +1 more source
Sub-pixel Mineral Mapping of Serpentine and Magnesite for Chromite Exploration, Using Hyperion (EO1) Images [PDF]
Abdasht chromite mine is located in the ultramafic complex of southern Iran, which has abundant chromite reserves such as Soghan, Esfandagheh, Faryab, etc.
Saeed Khojastehfar +2 more
doaj +1 more source
Kinetic model of carbonate dissolution in Martian meteorite ALH84001 [PDF]
The magnetites and sulfides located in the rims of carbonate globules in the Martian meteorite ALH84001 have been claimed as evidence of past life on Mars.
Humayun, Munir, Kopp, Robert E.
core +1 more source
Carbonate alteration of ophiolitic rocks in the Arabian–Nubian Shield of Egypt: sources and compositions of the carbonating fluid and implications for the formation of Au deposits [PDF]
Ultramafic portions of ophiolitic fragments in the Arabian–Nubian Shield (ANS) show pervasive carbonate alteration forming various degrees of carbonated serpentinites and listvenitic rocks.
Azer, Mokhles K. +9 more
core +2 more sources

