Results 1 to 10 of about 479 (172)

Miarolitic cavities in rapakivi granite on Hästholmen, Loviisa, southeastern Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1987
Miarolitic cavities are described from drill cores taken from rapakivi granite on Hästholmen, an island about 80 km east of Helsinki. The distribution of cavities between different textural types of rapakivi seems to favour the equigranular medium to ...
K. Lindqvist, V. Suominen
doaj   +5 more sources

Magmatic constraints on localization of natural stone deposits in the Vehmaa rapakivi granite batholith, southwestern Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 2011
The 1580–1570 Ma old Vehmaa rapakivi granite batholith was studied with the aim to define the geological constraints for localization of natural stone deposits in the batholith.
O. Selonen   +3 more
doaj   +2 more sources

Petrography and geochemistry of the topaz-bearing granite stocks in Artjärvi and Sääskjärvi, western margin of the Wiborg rapakivi granite batholith [PDF]

open access: yesBulletin of the Geological Society of Finland, 2002
The Artjärvi and Sääskjärvi granite stocks at the western margin of the Wiborg rapakivi batholith are multiphase rapakivi granite intrusions in which the most evolved phase is topaz-bearing granite.
S. Lukkari
doaj   +2 more sources

Sediment Characteristics in Stonewort <i>Chara Tomentosa</i> Assemblages. [PDF]

open access: yesEcol Evol
The study investigated sediment characteristics associated with Chara tomentosa. The results show that sediment grain size and the concentration of the dissolved phosphate in the porewater differ in the seafloor areas characterised by C. tomentosa from adjacent areas at similar depth, but without charophytes.
Puttonen I   +3 more
europepmc   +2 more sources

Layering in rapakivi granite, SW Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1974
Layering in rapakivi granite occurs locally in the islet Söderören, Åland, SW Finland. The layering consists of 3—5 cm thick, rhythmically repeated layers with high concentrations of biotite, hornblende, allanite and olivine.
C. Ehlers
doaj   +3 more sources

The Siipyy granite — a new rapakivi occurrence in Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1989
H. Idman
doaj   +2 more sources

Study supporting restoration of rapakivi granite in St. Petersburg

open access: yesResources Policy, 2022
Tuomas Sihvonen   +2 more
exaly   +2 more sources

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

Hydrogeological Characterization of Crystalline Bedrock Using Borehole Magnetic Resonance

open access: yesGroundwater, Volume 61, Issue 6, Page 793-815, November/December 2023., 2023
This study is one of the first to test the applicability of the borehole magnetic resonance (BMR) method in crystalline “hard rock” environment. The aim was to investigate whether the BMR measurements could constitute an effective method for investigating detailed permeability variations in the crystalline bedrock of the two study sites: Sakatti mining
Salla Eeva   +7 more
wiley   +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

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