Discovery of a Roman Quarry for Pozzolanic aggregates in the Euganean Hills Magmatic District, Northeast Italy: A stepwise archaeometric approach. [PDF]
Dilaria S +8 more
europepmc +1 more source
Shale-hosted vanadium occupation in typical silicate mineral structures. [PDF]
Fang-Yao H +6 more
europepmc +1 more source
Applications of machine learning algorithms in lithological mapping of Saint Katherine Neoproterozoic rocks in the South Sinai of Egypt using hyperspectral PRISMA data. [PDF]
Ali-Bik MW +4 more
europepmc +1 more source
Sustainable Ultrasound-Assisted Extraction and Recovery of Rare Earth Elements from Oil and Gas Drill Cuttings. [PDF]
Bez Fontana K +6 more
europepmc +1 more source
Visual analysis of deep learning semantic segmentation applied to petrographic thin sections. [PDF]
Morales J +8 more
europepmc +1 more source
Comprehensive hydrogeochemical characterization and seasonal water quality index analysis for sustainable groundwater management in Valliyur region, Southern Tamil Nadu, India. [PDF]
Promilton AAA +4 more
europepmc +1 more source
Energy evolution and catastrophic instability of excavated consequent slopes: A cusp catastrophe-based criterion and gradient-anchoring reinforcement strategy. [PDF]
Liu Z +7 more
europepmc +1 more source
Nomenclature of The Micas and “Biotite”
openaire +1 more source
Biotites and chlorites as interlayered biotite-chlorite crystal
En microscopie électronique à transmission et de haute résolution, il est fréquemment observé dans les biotites et les chlorites qu'il y a en fait mélange de feuillets élémentaires de biotite et de chlorite. D'après la terminologie courante, ces cristaux sont des interstratifications biotite-chlorite.
Olives Baños, Juan
openaire +3 more sources
Gneissic rock types are common in the coastal regions of the Baltic Sea and in the area of the planned deep repository at Olkiluoto. Based on experimental data and molecular modelling of mineral surfaces, the chemical reactions governing the sorption of Ni(II) and Eu(III) were interpreted using well-established thermodynamic sorption models.
Puukko, E. +6 more
core +5 more sources

