Anatomy of a diffuse cryptic suture zone: An example from the Bohemian Massif,European Variscides: Reply

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000085" target="_blank" >RIV/00025798:_____/14:00000085 - isvavai.cz</a>
Result on the web
<a href="http://geology.gsapubs.org/content/42/9/e347.full.pdf+html?sid=93a78dec-d902-4c46-ab05-2b23989dfbc5" target="_blank" >http://geology.gsapubs.org/content/42/9/e347.full.pdf+html?sid=93a78dec-d902-4c46-ab05-2b23989dfbc5</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1130/G36030Y.1" target="_blank" >10.1130/G36030Y.1</a>

Result language
angličtina
Original language name
Anatomy of a diffuse cryptic suture zone: An example from the Bohemian Massif,European Variscides: Reply
Original language description
Reply:Kroner and Romer (2014) argue that our model (Schulmann et al., 2014) is in conflict with the existence of the Rheic suture in the Bohemian Massif, and the 340 Ma age of ultrahigh-pressure (UHP) metamorphism. The model of the Rheic oceanic suture rimming the eastern margin of the Bohemian Massif suggests that the Brunia microcontinent is a part of Avalonia and formed a continuous Rhenohercynian Zone from southwest England to the Bohemian Massif.
Czech name
—
Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
—

Project
<a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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