Pennsylvanian-Permian deposits in northern Bohemia: a correlation with neighbouring basins and discussion of their formation and demise within the "Elbe Zone System"

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10169424" target="_blank" >RIV/00025798:_____/24:10169424 - isvavai.cz</a>

Výsledek na webu

<a href="https://gq.pgi.gov.pl/article/view/34211/25817" target="_blank" >https://gq.pgi.gov.pl/article/view/34211/25817</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Pennsylvanian-Permian deposits in northern Bohemia: a correlation with neighbouring basins and discussion of their formation and demise within the "Elbe Zone System"

Popis výsledku v původním jazyce

The crustal-scale shear-zones of the Bohemian Massif were recurrently active during the Late Paleozoic, as inferred from the depositional record of numerous penecontemporaneous basins distributed along NW-SE faults. This paper focuses on the correlation of sedimentary basins associated with Late Paleozoic reactivation of the NW-SE-trending Elbe Zone System, based on subsurface data from Permian outliers preserved along the Lusatian Fault in northern Bohemia. Comparison of the lithofacies development together with recently published geochronological data facilitates possible correlation to the Wei ss ig and Dohlen basins, and Bohemian basins, respectively. Stratigraphic dating and mutual correlation of the Late Paleozoic basins within the Elbe Zone allow comparison of their development and subsequent demise as a result of polyphase tectonic evolution of the northern Bohemian Massif. The Late Mississippian-Middle Pennsylvanian (similar to 330-310/305 Ma) late orogenic strike-slip tectonic movements were followed by extension related to orogenic collapse. This process was overtaken by intraplate extension by similar to 306/305 Ma at the latest. It has been suggested that the NW-SE faults (incl. Elbe Zone System) were reactivated in a strike-slipe regime during the Middle Pennsylvanian-early Permian (Moscovian-early Asselian; similar to 310-300/298 Ma), i.e., concurrently with the intra-plate extension. Further strike-slip reactivation of the NW-SE faults occurred during the early Permian (late Asselian-early Kungurian; similar to 297-283 Ma).

Název v anglickém jazyce

Pennsylvanian-Permian deposits in northern Bohemia: a correlation with neighbouring basins and discussion of their formation and demise within the "Elbe Zone System"

Popis výsledku anglicky

The crustal-scale shear-zones of the Bohemian Massif were recurrently active during the Late Paleozoic, as inferred from the depositional record of numerous penecontemporaneous basins distributed along NW-SE faults. This paper focuses on the correlation of sedimentary basins associated with Late Paleozoic reactivation of the NW-SE-trending Elbe Zone System, based on subsurface data from Permian outliers preserved along the Lusatian Fault in northern Bohemia. Comparison of the lithofacies development together with recently published geochronological data facilitates possible correlation to the Wei ss ig and Dohlen basins, and Bohemian basins, respectively. Stratigraphic dating and mutual correlation of the Late Paleozoic basins within the Elbe Zone allow comparison of their development and subsequent demise as a result of polyphase tectonic evolution of the northern Bohemian Massif. The Late Mississippian-Middle Pennsylvanian (similar to 330-310/305 Ma) late orogenic strike-slip tectonic movements were followed by extension related to orogenic collapse. This process was overtaken by intraplate extension by similar to 306/305 Ma at the latest. It has been suggested that the NW-SE faults (incl. Elbe Zone System) were reactivated in a strike-slipe regime during the Middle Pennsylvanian-early Permian (Moscovian-early Asselian; similar to 310-300/298 Ma), i.e., concurrently with the intra-plate extension. Further strike-slip reactivation of the NW-SE faults occurred during the early Permian (late Asselian-early Kungurian; similar to 297-283 Ma).

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GF22-11661K" target="_blank" >GF22-11661K: Integrovaná stratigrafie mladšího paleozoika ve východní části tropické Pangey</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Geological Quarterly

ISSN

1641-7291

e-ISSN

2082-5099

Svazek periodika

68

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

22

Strana od-do

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Kód UT WoS článku

001379870800001

EID výsledku v databázi Scopus

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