Metamorphic reprocessing of a serpentinized carbonate-bearing peridotite after detachment from the mantle wedge: A P-T path constrained from textures and phase diagrams in the system CaO-MgO-Al2O3-SiO2-CO2-H2O
Αποθετήριο DSpace/Manakin
JavaScript is disabled for your browser. Some features of this site may not work without it.
Metamorphic reprocessing of a serpentinized carbonate-bearing peridotite after detachment from the mantle wedge: A P-T path constrained from textures and phase diagrams in the system CaO-MgO-Al2O3-SiO2-CO2-H2O