Results 191 to 200 of about 16,574 (254)

Sustainable Concrete Production Using Granodiorite, Alkali Feldspar Granite, and Mafic Metavolcanic Rock Powders as Supplementary Cementitious Materials. [PDF]

Materials (Basel)
Faried AS, Fathy N, Morsi WM, Dawoud M, Mahmoud AS, Osman KM.   +5 more
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Influence of garnet and micas proportions in metamorphic rocks on laterite formation and variation in their road compaction parameters. [PDF]

Heliyon
Menye AJ, Mbessa M, Ngami PF, Bilong P.
europepmc   +1 more source

Temperature-induced microstructural evolution and fractal characteristics of high-enthalpy Chumathang granite for enhanced geothermal energy. [PDF]

Sci Rep
Singh M, Pandey SN, Chandra D, Singh N, Tripathi A, Yadav SK, Sass I, Srivastav AK, Saha SK.   +8 more
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P-T-t conditions of successive deformation stages during exhumation of orogenically thickened crust; a case study from the Aar Massif, Central Alps, Switzerland. [PDF]

Swiss J Geosci
Gnos E, Mullis J, Bergemann CA, Pettke T, Ricchi E, Schmitt AK.   +5 more
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Integrated geological datasets for the Zandrivierspoort Formation banded iron formation, Rhenosterkoppies Greenstone Belt, South Africa. [PDF]

Data Brief
Tibane LV, Mamba D, Nkosi ZH.
europepmc   +1 more source

Cooling rates and melt extraction timescales determined by diffusion chronometry on shallow crustal plutonic rocks. [PDF]

Contrib Mineral Petrol
Grocolas T, Müntener O, Bloch EM, Escrig S, Ulyanov A, Bouvier AS.   +5 more
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Assessment of critical mineral extraction from brines at Mount Meager, Southwestern BC, Canada. [PDF]

Sci Rep
Hormozzade Ghalati F, Motazedian D, Craven JA, Grasby SE, Tschirhart V.   +4 more
europepmc   +1 more source

A new activity model for biotite and its application. [PDF]

Contrib Mineral Petrol
Dachs E, Benisek A.
europepmc   +1 more source

Nomenclature of The Micas and “Biotite”

Journal of The Gemmological Society of Japan
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Magnetic interaction in biotites and oxidised biotites

Physics and Chemistry of Minerals, 1987
Mossbauer spectra of biotites (1) and (2) with relative iron concentrations ∼1:1·6 and of their oxidation products are recorded at 4 K in zero field and in applied fields up to 5 T. Magnetic susceptibility data are also reported. The results show that Fe III spins are in a ferromagnetic configuration in the c-plane in both biotites.
G. Longworth, M. G. Townsend, R. Provencher, H. Kodama   +3 more
openaire   +1 more source