Results 141 to 150 of about 3,307 (182)
Provenance, diagenesis, and depositional environment of Miocene Kamlial Formation, Azad Jammu and Kashmir, Sub Himalayas, Pakistan: Evidences from field observations and petrography. [PDF]
Khan M +6 more
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Effects and differences of various concentration techniques on the evolution of therapeutic components in Lushan geothermal water. [PDF]
Zhang B +8 more
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Bioleaching of uranium from ores and rocks using filamentous fungi. [PDF]
Bhatti TM, Tuovinen OH.
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Experimental evidence reveals the mobilization and mineralization processes of rare earth elements in carbonatites. [PDF]
Yuan X, Yang Z, Mayanovic RA, Hou Z.
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Geology of Ore Deposits, 2018
The chemical composition, crystal structure, and infrared (IR) spectrum of a hydrated CO3-bearing analog of manganoeudialyte from alkali pegmatites of the Konder pluton (Khabarovsk krai) are studied. The chemical composition of the mineral corresponds to the formula N[Na6.94H2O5.13(Y,REE)0.58.
A. S. Osipov +3 more
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The chemical composition, crystal structure, and infrared (IR) spectrum of a hydrated CO3-bearing analog of manganoeudialyte from alkali pegmatites of the Konder pluton (Khabarovsk krai) are studied. The chemical composition of the mineral corresponds to the formula N[Na6.94H2O5.13(Y,REE)0.58.
A. S. Osipov +3 more
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Trace element distributions between the perthite phases of alkali feldspars from pegmatites
Mineralogical Magazine, 1982AbstractThe distribution of various trace elements between the K-feldspar and albite phases of perthites from several pegmatites was determined by ion microprobe. Ranges in distribution coefficients (wt. % in K-feldspar/wt. % in albite) are: Li, 1.2–780; Mg, 0.2–1.1; P, 0.1–17; Ca, 0.02–1.6; Cs, 32–820; Ba, 24–284; Pb, 1.6–30; Fe, 0.3–0.7; Rb, 59–5505;
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Geology of Ore Deposits, 2014
Minerals of the gadolinite-(Y)-hingganite-(Y) series pertaining to the gadolinite-datolite group have been found in the alkali granite pegmatites of the Kola Peninsula. Gadolinite-(Y) is distinguished by its unique natural crystalline state. The unit-cell parameters of this mineral have elevated values as compared with those of gadolinite-(Y) from ...
L. M. Lyalina +4 more
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Minerals of the gadolinite-(Y)-hingganite-(Y) series pertaining to the gadolinite-datolite group have been found in the alkali granite pegmatites of the Kola Peninsula. Gadolinite-(Y) is distinguished by its unique natural crystalline state. The unit-cell parameters of this mineral have elevated values as compared with those of gadolinite-(Y) from ...
L. M. Lyalina +4 more
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Bulletin de Minéralogie, 1981
On étudie la minéralisation niobium˗tantale associée aux pegmatites de granite et aux roches granitiques alcalines d'Afrique et on présente une sélection de 124 analyses chimiques de divers minéraux de niobium et de tantale rencontrés au cours de cette étude.
von Knorring, Oleg, Fadipe, Akinola
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On étudie la minéralisation niobium˗tantale associée aux pegmatites de granite et aux roches granitiques alcalines d'Afrique et on présente une sélection de 124 analyses chimiques de divers minéraux de niobium et de tantale rencontrés au cours de cette étude.
von Knorring, Oleg, Fadipe, Akinola
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Geochimica et Cosmochimica Acta, 2014
Abstract This study presents a general model for the evaluation of Rayleigh fractional crystallisation as the principal differentiation mechanism in the formation of regionally zoned common and rare-element pegmatites. The magmatic evolution of these systems from a granitic source is reconstructed by means of alkali element and rare earth element ...
Niels Hulsbosch +4 more
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Abstract This study presents a general model for the evaluation of Rayleigh fractional crystallisation as the principal differentiation mechanism in the formation of regionally zoned common and rare-element pegmatites. The magmatic evolution of these systems from a granitic source is reconstructed by means of alkali element and rare earth element ...
Niels Hulsbosch +4 more
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Contributions to Mineralogy and Petrology, 1993
The ratios Na/Li, K/Li, Na/Cs and K/Cs have been calculated for exchange equilibria among the Li and Cs silicates spodumene, petalite, eucryptite, and pollucite, and the alkali feldspars albite and K-feldspar plus quartz, in pure water and in chloride solutions at temperatures from 100° to 700°C and pressures from 0.5 to 4 kbar, using available ...
Williams-Jones, A. E., Wood, S. A.
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The ratios Na/Li, K/Li, Na/Cs and K/Cs have been calculated for exchange equilibria among the Li and Cs silicates spodumene, petalite, eucryptite, and pollucite, and the alkali feldspars albite and K-feldspar plus quartz, in pure water and in chloride solutions at temperatures from 100° to 700°C and pressures from 0.5 to 4 kbar, using available ...
Williams-Jones, A. E., Wood, S. A.
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