Granitic pegmatites of the beryl-columbite subtype in the Tatric Superunit, Western Carpathians, Slovakia: Variscan age determination by in-situ LA-ICP-MS U-Pb dating of columbite-group minerals

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F24%3A10136549" target="_blank" >RIV/00023272:_____/24:10136549 - isvavai.cz</a>

Výsledek na webu

<a href="https://geologicacarpathica.com/browse/archive/?journal_article_no=33344" target="_blank" >https://geologicacarpathica.com/browse/archive/?journal_article_no=33344</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.31577/GeolCarp.2024.09" target="_blank" >10.31577/GeolCarp.2024.09</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Granitic pegmatites of the beryl-columbite subtype in the Tatric Superunit, Western Carpathians, Slovakia: Variscan age determination by in-situ LA-ICP-MS U-Pb dating of columbite-group minerals

Popis výsledku v původním jazyce

Accessory columbite-(Fe) to tantalite-(Fe) from three granitic pegmatites of the Tatric Superunit (Bratislava Massif of the Male Karpaty Mts., Bojna Massif of the Povazsky Inovec Mts. and Suchy Massif of the Strazovske Mts.) was used for dating by the in-situ LA-ICP-MS U-Pb method. The columbite-tantalite crystals were sampled from the most fractionated pegmatite dykes of the beryl-columbite subtype situated in the pre-Alpine, Paleozoic crystalline basement of the Tatric Superunit, Western Carpathians (western and central Slovakia). The obtained columbite-tantalite Concordia ages are as follows: 354.5 +/- 4.5 Ma (Jezuitske Lesy pegmatite, the Bratislava granite Massif), 360 +/- 5.0 Ma (Moravany nad Vahom, Striebornica Ridge pegmatite, the Bojna Massif), and 352 +/- 8.5 Ma (Liestany, Bystry Hill pegmatite, the Suchy Massif). The columbite-tantalite ages show Mid-Variscan formation of rare-element pegmatites from the Devonian/Carboniferous boundary to Tournaisian stage, which is coeval with the emplacement of cogenetic granites during the main phase of Variscan intracontinental subduction and collision. The obtained columbite-tantalite age interval of rare-element granitic pegmatites of the Tatric Superunit (similar to 360 to 350 Ma) is generally older than the ages of Be- and Li-rich rare-element pegmatites of the Moldanubian Superunit in the Bohemian Massif (similar to 340 to 320 Ma). The rare-element granitic pegmatites of the Austroalpine Superunit (Eastern Alps) are significantly younger (similar to 290 to 240 Ma) because they were formed in an extension regime during the Permian to Early Triassic post-Variscan orogenic collapse.

Název v anglickém jazyce

Granitic pegmatites of the beryl-columbite subtype in the Tatric Superunit, Western Carpathians, Slovakia: Variscan age determination by in-situ LA-ICP-MS U-Pb dating of columbite-group minerals

Popis výsledku anglicky

Accessory columbite-(Fe) to tantalite-(Fe) from three granitic pegmatites of the Tatric Superunit (Bratislava Massif of the Male Karpaty Mts., Bojna Massif of the Povazsky Inovec Mts. and Suchy Massif of the Strazovske Mts.) was used for dating by the in-situ LA-ICP-MS U-Pb method. The columbite-tantalite crystals were sampled from the most fractionated pegmatite dykes of the beryl-columbite subtype situated in the pre-Alpine, Paleozoic crystalline basement of the Tatric Superunit, Western Carpathians (western and central Slovakia). The obtained columbite-tantalite Concordia ages are as follows: 354.5 +/- 4.5 Ma (Jezuitske Lesy pegmatite, the Bratislava granite Massif), 360 +/- 5.0 Ma (Moravany nad Vahom, Striebornica Ridge pegmatite, the Bojna Massif), and 352 +/- 8.5 Ma (Liestany, Bystry Hill pegmatite, the Suchy Massif). The columbite-tantalite ages show Mid-Variscan formation of rare-element pegmatites from the Devonian/Carboniferous boundary to Tournaisian stage, which is coeval with the emplacement of cogenetic granites during the main phase of Variscan intracontinental subduction and collision. The obtained columbite-tantalite age interval of rare-element granitic pegmatites of the Tatric Superunit (similar to 360 to 350 Ma) is generally older than the ages of Be- and Li-rich rare-element pegmatites of the Moldanubian Superunit in the Bohemian Massif (similar to 340 to 320 Ma). The rare-element granitic pegmatites of the Austroalpine Superunit (Eastern Alps) are significantly younger (similar to 290 to 240 Ma) because they were formed in an extension regime during the Permian to Early Triassic post-Variscan orogenic collapse.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Geologica Carpathica

ISSN

1335-0552

e-ISSN

—

Svazek periodika

75

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

13

Strana od-do

157-169

Kód UT WoS článku

001309144600001

EID výsledku v databázi Scopus

—