How old is the Třebíč durbachitic Pluton? Reply to Comment on 'Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Třebíč Pluton, the largest durbachitic body in the Bohemian Massif' by Schaltegger et al

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F21%3A00000037" target="_blank" >RIV/00025798:_____/21:00000037 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/21:00542148 RIV/00216208:11310/21:10428696
Result on the web
<a href="https://link.springer.com/article/10.1007%2Fs00531-020-01977-8" target="_blank" >https://link.springer.com/article/10.1007%2Fs00531-020-01977-8</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00531-020-01977-8" target="_blank" >10.1007/s00531-020-01977-8</a>

Result language
angličtina
Original language name
How old is the Třebíč durbachitic Pluton? Reply to Comment on 'Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Třebíč Pluton, the largest durbachitic body in the Bohemian Massif' by Schaltegger et al
Original language description
New re-evaluation of our U–Pb LA-ICP-MS data for strongly porphyritic melagranite 1322 from Petráveč (NE part of the Variscan ultrapotassic Třebíč Pluton, Moldanubian Zone of the Bohemian Massif) gives a weighted mean 207Pb/235U age of 335 ± 3 Ma (2sigma). This, together with our previous U–Pb LA-ICP-MS zircon age of 335 ± 3 Ma and CA-ID-TIMS zircon age of 335.127 ± 0.11 Ma newly acquired by Schaltegger et al. from the central part of the Třebíč body pin-point its emplacement age to 335 Ma. Importantly, this datum constrains the oblique underthrusting of Brunia microcontinent, subvertical shortening and development of flat fabric in the Moldanubian Zone. Precise timing of the other Moldanubian durbachitic intrusions remains open to discussion.
Czech name
—
Czech description
—

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

Project
<a href="/en/project/GA18-24378S" target="_blank" >GA18-24378S: Petrogenesis of (ultra-)potassic magmas in the European Variscides – implications for development of collisional orogens and crustal growth models</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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