Magnetic fabric of granitic composite pluton of the Velka Fatra Mountains (Western Carpathians, Slovakia): A Variscan remnant within the Alpine edifice?

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F09%3A10001049" target="_blank" >RIV/00216208:11310/09:10001049 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic fabric of granitic composite pluton of the Velka Fatra Mountains (Western Carpathians, Slovakia): A Variscan remnant within the Alpine edifice?

Popis výsledku v původním jazyce

The AMS study has been performed on various types of the basement - Variscan granitic and surrounding - Mesozoic sedimentary rocks in the Vel'ka Fatra Mountains, Tatric Superunit of the Central Western Carpathians. The Vel'ka Fatra Mts. provides good opportunity for AMS study because of composite S-type and I-type granite character of pluton and clear relations to Mesozoic sedimentary rocks in the cover and nappe positions. The granitic massif consists of the three types of weakly magnetic peraluminousgranites (350 - 340 Ma in age), ranging from two-mica granites to biotite granodiorites in composition and carrying accessory monazite and ilmenite; whereby they resemble common S-type and/or Ilmenite Series granite.

Název v anglickém jazyce

Magnetic fabric of granitic composite pluton of the Velka Fatra Mountains (Western Carpathians, Slovakia): A Variscan remnant within the Alpine edifice?

Popis výsledku anglicky

The AMS study has been performed on various types of the basement - Variscan granitic and surrounding - Mesozoic sedimentary rocks in the Vel'ka Fatra Mountains, Tatric Superunit of the Central Western Carpathians. The Vel'ka Fatra Mts. provides good opportunity for AMS study because of composite S-type and I-type granite character of pluton and clear relations to Mesozoic sedimentary rocks in the cover and nappe positions. The granitic massif consists of the three types of weakly magnetic peraluminousgranites (350 - 340 Ma in age), ranging from two-mica granites to biotite granodiorites in composition and carrying accessory monazite and ilmenite; whereby they resemble common S-type and/or Ilmenite Series granite.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

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

Název periodika

GEODINAMICA ACTA

ISSN

0985-3111

e-ISSN

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Svazek periodika

22

Číslo periodika v rámci svazku

1-3

Stát vydavatele periodika

FR - Francouzská republika

Počet stran výsledku

17

Strana od-do

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Kód UT WoS článku

000272690200004

EID výsledku v databázi Scopus

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