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Fluid pathways within shallow-generated damage zones of strike-slip faults – evidence of map-scale faulting in a continental environment, SW Permo-Mesozoic cover of the Late Palaeozoic Holy Cross Mountains Fold Belt, Poland

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cris.lastimport.scopus2024-02-12T20:33:57Z
dc.abstract.enThe damage zones of exhumed strike-slip faults dissecting Jurassic carbonates in the south-western part of the Late Palaeozoic Holy Cross Mountains Fold Belt reveal second-order faults and fractures infilled with syntectonic calcite. The subsequent development of a structural pattern of microscopic fault-related structures and calcite infillings reflects the activity of strike-slip faults that began in the Late Cretaceous (Late Maastrichtian) and lasted until the early Miocene (Langhian). The fabric of the syntectonic veins provides insights into the evolution of the permeable fault-related structures that were the main pathways for fluid flow during fault activity. Microstructural study of calcite veins coupled with stable isotope and fluid inclusion data indicates that calcite precipitated primarily in a rock-buffered system related to strike-slip fault movement, and secondarily in a partly open system related to the local activity of the releasing Chmielnik stepover or the uplift of the area. The presence of meteoric fluids descending from the surface into damage zones suggest that the strike-slip faulting might have taken place in a nonmarine, continental environment.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorRybak-Ostrowska, Barbara
dc.contributor.authorKonon, Andrzej
dc.contributor.authorHurai, Vratislav
dc.contributor.authorBojanowski, Maciej
dc.contributor.authorKonon, Agnieszka
dc.contributor.authorWyglądała, Michał
dc.date.accessioned2024-01-25T01:13:50Z
dc.date.available2024-01-25T01:13:50Z
dc.date.issued2020
dc.description.accesstimeAT_PUBLICATION
dc.description.financePublikacja bezkosztowa
dc.description.number1
dc.description.versionFINAL_PUBLISHED
dc.description.volume70
dc.identifier.doi10.24425/AGP.2019.126454
dc.identifier.issn0001-5709
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/107294
dc.identifier.weblinkhttps://geojournals.pgi.gov.pl/agp/article/view/27933
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofActa Geologica Polonica
dc.relation.pages1-29
dc.rightsCC-BY
dc.sciencecloudnosend
dc.titleFluid pathways within shallow-generated damage zones of strike-slip faults – evidence of map-scale faulting in a continental environment, SW Permo-Mesozoic cover of the Late Palaeozoic Holy Cross Mountains Fold Belt, Poland
dc.typeJournalArticle
dspace.entity.typePublication