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Wodginite as an indicator mineral of tantalum-bearing pegmatites and granites

open access: yesЗаписки Горного института, 2023
In the composition of tantalum-niobates, the tin-bearing wodginite group minerals (WGM) were found: wod-ginite, titanowodginite, ferrowodginite, ferrotitanowodginite, lithiowodginite, tantalowodginite, “wolframowodginite”.
Viktor I. Alekseev
doaj   +1 more source

Rare metal granites and related rocks of the Ukrainian shield [PDF]

open access: yesBulletin of the Geological Society of Finland, 1993
Two rare metal leucocratic granites, Perga and Kamennaya complexes, can be distinquished on the Ukrainian shield. The Perga complex consists of medium- and coarse-grained, mainly porphyric, biotite, riebeckite and aegirine granites, granite porphyries ...
K.Y. Esipchuk   +2 more
doaj   +1 more source

Gravimetric and magnetic characterization of structural controls on Sn-W ore deposits. A case study in the san finx deposit (A Coruña)

open access: yesGeogaceta, 2022
Critical raw materials are essential for the development of our society. However, most shallow ores have already been exploited and only deep targets remain unexplored. This work aims to apply indirect geophysical techniques to the San Finx Sn-W deposit
Alberto Santamaría Barragán   +6 more
doaj   +1 more source

Petrogenesis of the Kanker Granites From the Bastar Craton: Implications for Crustal Growth and Evolution During the Archean-Proterozoic Transition

open access: yesFrontiers in Earth Science, 2020
Archean-Proterozoic boundary represents a significant transitional phase in the Earth's history. Bastar Craton is one of the major Archean cratons in the Indian subcontinent with voluminous granites, supracrustal rocks, and tectonic belts.
Ajay Dev Asokan   +4 more
doaj   +1 more source

The occurrence of rare earth elements in some Finnish mires [PDF]

open access: yesBulletin of the Geological Society of Finland, 1995
The content of the more abundant rare earths (RE) (Y, La, Ce, Pr, Nd and Sm) in the ash of 399 peat samples from 26 Finnish mires was determined by X-ray fluorescence spectrometry.
I. Yliruokanen, S. Lehto
doaj   +1 more source

Geochronology of the Suomenniemi rapakivi granite complex revisited: Implications of point-specific errors on zircon U-Pb and refined λ87 on whole-rock Rb-Sr [PDF]

open access: yesBulletin of the Geological Society of Finland, 2015
Multi-grain isotope dilution and secondary ion microprobe zircon U-Pb as well as wholerock Rb-Sr isotope dilution data on the late Paleoproterozoic Suomenniemi rapakivi granite complex (exposed on the northern flank of the Wiborg batholith in ...
O.T. Rämö, I. Mänttäri
doaj   +1 more source

A specialized topaz-bearing rapakivi granite and associated mineralized greisen in the Ahvenisto complex, SE Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1991
The Ahvenisto rapakivi complex is a satellite northwest of the large Wiborg rapakivi batholith in Southeastern Finland. The rapakivi rocks are surrounded by rapakivi-age gabbros, anorthosites, monzodiorites and diabases.
P. Edén
doaj   +1 more source

Fluid inclusions in cavity quartz crystals in rapakivi from Luumäki, southeastern Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1991
Fluid inclusions in selected cavity quartz crystals in rapakivi granite from Luumäki, southeastern Finland, were studied by microthermometric methods.
M. Poutiainen
doaj   +1 more source

Tirekhtyakh, Arga-Ynnakh-Khai and Kester intrusive complexes based on the materials of GDP-200 on the territory of sheets Q-53-IX, X

open access: yesРуды и металлы, 2022
The structural position, petrographic composition, petro- and geochemical features of amphibole-biotite, biotite and amblygonite-lepidolite granitoid of the study area are characterized.
Larisa G. Vdovina
doaj   +1 more source

Distribution of rare earth elements in Ruska Poliana granites and accessory fluorites

open access: yesМінеральні ресурси України, 2019
Fluorite is one of the main concentrators of rare earth elements (REE) in the granites of the Ruska Polіana massif of the Korsun-Novomyrhorod pluton of the Ukrainian Shield. Despite its distribution in the granites of the massif, the geochemical features
O. M. Ponomarenko   +4 more
doaj   +1 more source

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