Continuous magma mixing and cumulate separation in the High Tatra Mountains open system granitoid intrusion, Western Carpathians (Poland/Slovakia): a textural and geochemical study

Gawęda, Aleksandra; Szopa, Krzysztof; Włodyka, Roman; Burda, Jolanta; Crowley, Quentin; Sikorska, Magdalena

doi:10.24425/agp.2019.126447

Artykuł - szczegóły

Tytuł artykułu

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

Treść / Zawartość

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Identyfikatory

DOI

10.24425/agp.2019.126447

Warianty tytułu

Języki publikacji

Abstrakty

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.

Słowa kluczowe

Tatra granitoids magma mixing cumulate formation

granitoidy tatrzańskie mieszanie magmy łączenie formacji

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2019

Tom

Vol. 69, no. 4

Strony

549--570

Opis fizyczny

Bibliogr. 62 poz. rys., tab., wykr.

Twórcy

autor

Gawęda Aleksandra

aleksandra.gaweda@us.edu.pl

Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland

autor

Szopa Krzysztof

Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland

autor

Włodyka Roman

Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland

autor

Burda Jolanta

Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland

autor

Crowley Quentin

Department of Geology, School of Natural Sciences, Trinity College Dublin, Dublin 2, Ireland

autor

Sikorska Magdalena

Polish Geological Institute-National Research Institute, ul. Rakowiecka 4, Warsaw, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-095a43c6-e12c-4377-9110-5062d9ce91a9