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Origin of the pegmatite veins within the skarn body at Vevčice near Znojmo (Gfohl Unit, Moldanubian Zone)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F17%3A00475498" target="_blank" >RIV/67985831:_____/17:00475498 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216305:26110/17:PU123575 RIV/00025798:_____/17:00000039 RIV/00094862:_____/17:N0000181

  • Result on the web

    <a href="http://dx.doi.org/10.3190/jgeosci.234" target="_blank" >http://dx.doi.org/10.3190/jgeosci.234</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3190/jgeosci.234" target="_blank" >10.3190/jgeosci.234</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Origin of the pegmatite veins within the skarn body at Vevčice near Znojmo (Gfohl Unit, Moldanubian Zone)

  • Original language description

    The lower crustal Gfohl Unit (Moldanubian Zone of the Bohemian Massif) consists of various felsic orthogneisses to migmatites (the so-called Gfohl gneiss) that are conunonly associated with the high-pressure felsic granulites, serpentinized gamet/spinel peridotites, garnet pyroxenites, eclogites and skanis. The relatively small skarn bodies at Vevcice in southern Moravia have the prevailing assemblage of medium- to coarse-grained granoblastic clinopyroxene + garnet +/- amphibole +/- epidote. The skarn is cut by narrow veins of diorite pegmatite (SiO2 = 46-56 wt. %) which is geochemically distinct from granitic melt generated by migmatization of surrounding orthogneisses. Major pegmatite minerals are plagioclase (An(15-14)), amphibole (K-rich hastingsite and potassic-hastingsite) and quartz, accompanied by minor K-feldspar, garnet, allanite-epidote, clinopyroxene, and accessory titanite. The pegmatites are characterized by high contents of Fe2O3tot, (11.2-17.5 wt. %), Ca2O (7.5-10.11 wt. %), Na2O (2.9-3.3 wt. %) and low contents of MgO (1.4-1.6 wt. %), K2O (1.2-1.6 wt. %), Rb (43-86 ppm). Whole-rock and mineral chemistry of diorite pegmatites are consistent with their origin as a product of melt infiltration from surrounding migmatites and subsequent contamination by the country-rock skarn, with or without, fractional crystallization/crystal accumulation. Similarity in composition of amphiboles in the skarn and in the pegmatite can indicate formation under similar conditions, at c. 750 degrees C and 0.7-0.8 GPa.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/LO1408" target="_blank" >LO1408: AdMaS UP – Advanced Building Materials, Structures and Technologies</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2017

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of Geosciences

  • ISSN

    1802-6222

  • e-ISSN

  • Volume of the periodical

    62

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    23

  • Pages from-to

    1-23

  • UT code for WoS article

    000400030700001

  • EID of the result in the Scopus database

    2-s2.0-85018366428