Reply to discussion on 'Oroclinal arcs of the Variscan Belt: a consequence of transpression during the consolidation of Pangaea', by Martínez Catalán et al. 2024 (JGS, 181, jgs2024-007)

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F25%3A10169678" target="_blank" >RIV/00025798:_____/25:10169678 - isvavai.cz</a>
Result on the web
<a href="https://doi.org/10.1144/jgs2025-131" target="_blank" >https://doi.org/10.1144/jgs2025-131</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1144/jgs2025-131" target="_blank" >10.1144/jgs2025-131</a>

Result language
angličtina
Original language name
Reply to discussion on 'Oroclinal arcs of the Variscan Belt: a consequence of transpression during the consolidation of Pangaea', by Martínez Catalán et al. 2024 (JGS, 181, jgs2024-007)
Original language description
The discussion by Casas et al. (2025) on our paper about the oroclinal arcs in the Variscan Belt (Martínez Catalán et al. 2024) is welcome because it allows us to update some of our ideas in the light of recent new results. As the discussion only addresses the Ibero- Armorican Arc (IAA), we will also focus on this structural feature, dealing with (1) the geometry of the arc, (2) the structures involved and their mechanical constraints and (3) the timing of arc development.
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/GA23-08249S" target="_blank" >GA23-08249S: Origin of the relaminant in the Bohemian Massif during the Variscan orogeny</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2025
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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