DC pole | Wartość | Język |
dc.contributor.author | Botor, Dariusz | - |
dc.contributor.author | Toboła, Tomasz | - |
dc.contributor.author | Jelonek, Iwona | - |
dc.date.accessioned | 2018-03-12T08:41:53Z | - |
dc.date.available | 2018-03-12T08:41:53Z | - |
dc.date.issued | 2017 | - |
dc.identifier.citation | Annales Societatis Geologorum Poloniae, vol. 87 (2017), s. 13–40 | pl_PL |
dc.identifier.issn | 0208-9068 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/1073 | - |
dc.description.abstract | Raman microspectroscopy of organic matter, vitrinite reflectance and fluid inclusion data were used to
reconstruct the thermal history in the lower Carboniferous accretionary prism of the Culm Basin in the Nízký
Jeseník Mts. (NE Bohemian Massif). The model involves the Variscan (mid–late Carboniferous) burial diagenesis,
which was overprinted by a post-Variscan, probably Permian and/or early Mesozoic, thermal pulse(s) in
its central and western parts. The latter may have been related to advective heat transport and the circulation of hot
fluids. In the siliciclastic rocks of the Culm Basin, the maximum palaeotemperatures varied from ~200 ± 30 °C in
the E (in the Hradec-Kyjovice Formation) to ~350 ± 30 °C in the NW (in the Andìlská Hora Formation). | pl_PL |
dc.language.iso | en | pl_PL |
dc.subject | Raman spectroscopy | pl_PL |
dc.subject | carbonaceous material | pl_PL |
dc.subject | maximum temperature | pl_PL |
dc.subject | fluid inclusions | pl_PL |
dc.subject | vitrinite reflectance | pl_PL |
dc.subject | Culm Basin | pl_PL |
dc.subject | Moravo-Silesian Fold and Thrust Belt | pl_PL |
dc.title | Thermal history of the lower Carboniferous Culm Basin in the Nizky Jesenik Mts. (NE Bohemian Massif, Czech Republic and Poland) | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.relation.journal | Annales Societatis Geologorum Poloniae | pl_PL |
dc.identifier.doi | 10.14241/asgp.2017.002 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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