Results 51 to 60 of about 202 (128)
Abstract Granulites from the Narryer Terrane in the northern Yilgarn Craton, Australia, record evidence for high to ultrahigh thermal gradients during the Meso–Neoarchean. U–Pb zircon ages reflect a complex history of high‐grade, prolonged and poly‐phase metamorphism, with evidence for several thermal pulses at ca. 2745–2725, ca.
Naomi M. Tucker +7 more
wiley +1 more source
Abstract The Western Gneiss Region (WGR) is a Precambrian basement domain in the Scandinavian Caledonides and one of the world's largest high‐ and ultrahigh‐pressure terranes. The south–central WGR underwent regional eclogite facies metamorphism 415–400 Ma ago when Baltica subducted beneath Laurentia, during the Scandian orogeny.
Charlotte Möller +4 more
wiley +1 more source
Abstract The oldest known evolved (felsic) rocks on Earth (c. 4.03 Ga) are found in the Acasta Gneiss Complex (AGC) in north‐western Canada and represent a fundamental keystone in unravelling the geological processes governing crustal growth and differentiation during the Hadean and early Archean.
Jonas Kaempf +6 more
wiley +1 more source
Abstract Reconstructing the original geometry of a high‐pressure tectonic unit is challenging but important to understand the mechanisms of mountain building. While a single nappe is subducted and exhumed, nappe‐internal thrusts may disrupt it into several subunits.
Alexandre Peillod +11 more
wiley +1 more source
Effect of mineralogical variations on physico-mechanical and thermal properties of granitic rocks. [PDF]
Lasheen ESR, Rashwan MA, Azer MK.
europepmc +1 more source
Investigating the geochemical behavior and exploration potential of lithium in brines; a case study of Bam salt plug, Zagros Zone, southern Iran. [PDF]
Bazamad M +3 more
europepmc +1 more source
Hydrothermal enrichment of lithium in intracaldera illite-bearing claystones. [PDF]
Benson TR, Coble MA, Dilles JH.
europepmc +1 more source
Transition from carbonatitic magmas to hydrothermal brines: Continuous dilution or fluid exsolution? [PDF]
Yuan X, Zhong R, Xiong X, Gao J, Ma Y.
europepmc +1 more source
According to the literature, the pegmatites of Madeira granite, located in the mining district of Pitinga (Amazonas, Brazil), belong to the albite granite facies. Previous studies have proposed that these pegmatitic bodies are associated with N320/60SW oriented faults and are rich in rare earth elements (REE). Due to this, the characterization of these
PALUDO, Carina M. +3 more
openaire +1 more source
Characteristics of Thermal Parameters and Some Physical Properties of Mineral Eutectic Type: Petalite-Alkali Feldspars. [PDF]
Stempkowska A.
europepmc +1 more source

