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

Result code in 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>

Result on the web

<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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Result language

angličtina

Original language name

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

Original language description

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).

Czech name

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Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

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OECD FORD branch

10505 - Geology

Project

<a href="/en/project/GF22-11661K" target="_blank" >GF22-11661K: Towards integrated stratigraphy of the Late Paleozoic in eastern equatorial Pangea</a><br>

Continuities

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

Publication year

2024

Confidentiality

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

Name of the periodical

Geological Quarterly

ISSN

1641-7291

e-ISSN

2082-5099

Volume of the periodical

68

Issue of the periodical within the volume

4

Country of publishing house

PL - POLAND

Number of pages

22

Pages from-to

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UT code for WoS article

001379870800001

EID of the result in the Scopus database

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