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Wyszukujesz frazę "granitoidy" wg kryterium: Wszystkie pola


Wyświetlanie 1-4 z 4
Tytuł:
Native silver in the eastern part of the Karkonosze granitoid pluton, Lower Silesia, Poland
Autorzy:
Kozłowski, Andrzej
Matyszczak, Witold
Powiązania:
https://bibliotekanauki.pl/articles/27323964.pdf
Data publikacji:
2023
Wydawca:
Polska Akademia Nauk. Czasopisma i Monografie PAN
Tematy:
native silver
fluid inclusions
granitoid
Karkonosze pluton
srebro rodzime
inkluzja fluidalna
granitoidy
pluton Karkonoszy
Opis:
This article describes silver specimens of the size of tenths to a few millimetres, found in small pegmatites and quartz veinlets of the porphyritic granitoid area in 22 sites in the eastern part of the Variscan granitoid Karkonosze pluton, from 20 of which native silver occurrences were previously not known. The sites are scattered on the whole surface of the granitoid. The native silver occurred in wire, rod, platy, dendritic, anhedral granular and euhedral cubic and octahedral habits; in some specimens twins and fenster faces were also found. Associated with native silver small amounts of acanthite crystallized commonly, sometimes apparently formed by sulphur diffusion into silver. Inclusions of native gold, electrum, galena, chalcopyrite and pyrite occurred in the native silver. The parent fluids of the specimens were epithermal, because the homogenization temperature (Th) of inclusions in quartz, calcite and cleavelandite that were the host minerals of the native silver was generally 91–165ºC and for individual samples the Th range was 4–11ºC. The total salinity of the fluid was 2.4–7.2 wt. % with Na and Ca (hydro)carbonates as the main dissolved components and admixtures of K, Mg, Fe, Al, S, Cl and F. The parent granitoid contains Ag in trace amounts (0.034–0.056 ppm) and was probably the source of this element for the crystals of native silver. Migration of Ag was made easier by the presence of fluoride ions in fluids.
Źródło:
Acta Geologica Polonica; 2023, 73, 2; 223--245
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Fluorite and related fluids in the Karkonosze granitoid pluton, SW Poland
Autorzy:
Kozłowski, Andrzej
Matyszczak, Witold
Powiązania:
https://bibliotekanauki.pl/articles/2023996.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Karkonosze pluton
Variscan granitoids
pegmatite
fluorite
fluid inclusions
inclusion alterations
post-magmatic fluids
pluton Karkonoszy
waryscyjskie granitoidy
pegmatyt
fluoryt
inkluzje fluidalne
Opis:
Fluorite mineralization was studied in the Variscan granitoid Karkonosze pluton in the northern part of the Bohemian massif (Lower Silesia, Poland). Fluid inclusions in fluorite and quartz were investigated by the following methods: heating and freezing on an immersion microscope stage, spectrophotometric and electron probe analysis, calcination and water leachate. The parent fluids of fluorite were of the Na-Ca-Cl type with a low CO₂ content. The fluoride ions had sources in the pluton and in its host rocks. Fluid inclusion observations provide evidence of various post-formation alteration. such as refilling, partition, cracking, migration, expulsion or vacuole modification from irregular to cubic habit. A final model of fluorite origin and parent fluid evolution is presented.
Źródło:
Acta Geologica Polonica; 2022, 72, 1; 9--31
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Th-U-total Pb timing constraints on the emplacement of the granitoid pluton of Stolpen, Germany
Autorzy:
Lisowiec, K.
Budzyń, B.
Słaby, E.
Schulz, B.
Renno, A. D.
Powiązania:
https://bibliotekanauki.pl/articles/950363.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Th-U-Pb chemical dating
Lusatian Granodiorite Complex
Stolpen Granite
Variscan granitoids
Łużyce
granodioryt
kompleks
granit
waryscyjskie granitoidy
Opis:
Monazite from the Stolpen monzogranite (SE Germany) was studied to constrain the Th-U-total Pb age of pluton formation. Monazite grains demonstrate subtle to distinct patchy zoning related to slight compositional variations. Textural and compositional characteristics indicate that the monazite formed in a single magmatic event in a slightly heterogeneous system, and was only weakly affected by secondary alteration, which did not disturb the Th-U-Pb system. Chemical dating of the monazite gave a consistent age of 299 ± 1.7 Ma. The current study presents the first geochronological data for the Stolpen granite. It provides evidence that Stolpen is the youngest Variscan granitic intrusion in the Lusatian Granodiorite Complex and indicates that magmatic activity related to post-collisional extension in this region lasted at least 5my longer than previously assumed.
Źródło:
Acta Geologica Polonica; 2014, 64, 4; 457-472
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Continuous magma mixing and cumulate separation in the High Tatra Mountains open system granitoid intrusion, Western Carpathians (Poland/Slovakia): a textural and geochemical study
Autorzy:
Gawęda, Aleksandra
Szopa, Krzysztof
Włodyka, Roman
Burda, Jolanta
Crowley, Quentin
Sikorska, Magdalena
Powiązania:
https://bibliotekanauki.pl/articles/138682.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Tatra granitoids
magma mixing
cumulate formation
granitoidy tatrzańskie
mieszanie magmy
łączenie formacji
Opis:
In this study the formation of the polygenetic High Tatra granitoid magma is discussed. Felsic and mafic magma mixing and mingling processes occurred in all magma batches composing the pluton and are documented by the typical textural assemblages, which include: mafic microgranular enclaves (MME), mafic clots, felsic clots, quartz-plagioclase-titanite ocelli, biotite-quartz ocelli, poikilitic plagioclase crystals, chemically zoned K-feldspar phenocrysts with inclusion zones and calcic spikes in zoned plagioclase. Geochemical modelling indicates the predominance of the felsic component in subsequent magma batches, however, the mantle origin of the admixed magma input is suggested on the basis of geochemical and Rb-Sr, Sm-Nd and Pb isotopic data. Magma mixing is considered to be a first-order magmatic process, causing the magma diversification. The cumulate formation and the squeezing of remnant melt by filter pressing points to fractional crystallization acting as a second-order magmatic process.
Źródło:
Acta Geologica Polonica; 2019, 69, 4; 549-570
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-4 z 4

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