Last stage of Variscan granitoid magmatism in the Strzelin Massif (SW Poland) : petrology and age of the biotite-muscovite granites

Oberc-Dziedzic, T.; Kryza, R.; Pin, C.

doi:10.7306/gq.1248

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Tytuł artykułu

Last stage of Variscan granitoid magmatism in the Strzelin Massif (SW Poland) : petrology and age of the biotite-muscovite granites

Autorzy

Oberc-Dziedzic T. , Kryza R. , Pin C.

Treść / Zawartość

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Dziedzic_T_Last stage_Geol. Quart_Vol.59_No 4_2015.pdf

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DOI

10.7306/gq.1248

Warianty tytułu

Języki publikacji

Abstrakty

New petrographic and geochemical data show some differences between Variscan Bt-Ms granites occurring either as small plutons or dykes in the Strzelin Massif (SW Poland). The granites of the Gromnik and Górka Sobocka plutons are rich in micas and crystallized from "wet" magmas; the granites in the dykes and in the Gębczyce pluton are mica-poorer and cordierite-bearing rocks, derived from “dryer” magmas. The lower initial eNd values in the Bt-Ms granites of the dykes, compared with those in the plutons, reflect a more "crustal" signature of the former, possibly due to local crustal assimilation, via AFC, shortly before emplacement. Much more radiogenic initial ⁸⁷Sr/⁸⁶Sr ratios in the dykes, up to 0.726, further suggest the involvement of extraneous, hydrous crustal fluids enriched in ⁸⁷Sr during the evolution of late-stage magma derivatives. The new U-Pb SHRIMP zircon age of 296 ± 6 Ma for the Gębczyce Bt-Ms granite shows that this body belongs to the third stage of magmatism in the Strzelin Massif. The U-Pb SHRIMP zircon data for the Bt-Ms granite dykes provide ages similar to those of their host rocks: c. 295 Ma for the Gęsiniec tonalite and the enclosed Bt-Ms granite, and c. 285 Ma for the Strzelin biotite granite and its Bt-Ms granite dykes. These new data from peraluminous rock-types complement our previous studies focused on the tonalites, granodiorites and biotite granites, and shed light on the late-stage igneous evolution of the Strzelin Massif.

Słowa kluczowe

biotite-muscovite granite cordierite nodules SHRIMP zircon ages Variscan granitoids Strzelin Massif

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2015

Tom

Vol. 59, No. 4

Strony

718--737

Opis fizyczny

Bibliogr. 64 poz., rys., tab., wykr.

Twórcy

autor

Oberc-Dziedzic T.

Univer sity of Wrocław, Institute of Geological Sciences, Plac M. Borna 9, 50-204 Wrocław, Poland

autor

Kryza R.

Univer sity of Wrocław, Institute of Geological Sciences, Plac M. Borna 9, 50-204 Wrocław, Poland

autor

Pin C.

Université Blaise Pascal, Département de Géologie, CNRS, 5 rue Kessler, 63038 Clermont-Ferrand, Cedex, France

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