Szczegóły publikacji
Opis bibliograficzny
Burial and thermal history of the Lower Palaeozoic petroleum source rocks at the SW margin of the East European Craton (Poland) / Dariusz BOTOR, Jan GOLONKA, Aneta A. Anczkiewicz, István Dunkl, Bartosz PAPIERNIK, Justyna ZAJĄC, Piotr GUZY // Annales Societatis Geologorum Poloniae ; ISSN 0208-9068. — 2019 — vol. 89 no. 2, s. 121–152. — Bibliogr. s. 146–152, Abstr.
Autorzy (7)
- AGHBotor Dariusz
- AGHGolonka Jan
- Anczkiewicz Aneta A.
- Dunkl István
- AGHPapiernik Bartosz
- AGHZając Justyna
- AGHGuzy Piotr
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 125917 |
|---|---|
| Data dodania do BaDAP | 2019-12-20 |
| Tekst źródłowy | URL |
| DOI | 10.14241/asgp.2019.12 |
| Rok publikacji | 2019 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Annales Societatis Geologorum Poloniae |
Abstract
Thermal maturity modelling was carried out in over sixty wells along the SW margin of the East European Craton (EEC). The burial and thermal history modelling of the EEC, using thermochronological data, allowed the construction of burial history maps showing its geological development in the Phanerozoic. These results have proved that the Ordovician and Silurian source rocks occurring at the SW margin of the EEC reached a maximum palaeotemperature in the Palaeozoic, mainly during Devonian-Carboniferous time and at the latest during the Silurian in the most westerly part of this margin, along the Teisseyre-Tornquist Zone. In Mesozoic and Cainozoic time, the Ordovician and Silurian strata generally were subjected to cooling or to very minor heating, certainly below the Variscan level. The maximum burial and maximum temperature of the Ediacaran-Lower Palaeozoic strata were reached during the Early Carboniferous in the Baltic Basin and during the Late Carboniferous in the Lublin area, and even in the Early Permian in the SE corner of the Lublin Basin. Thus, the main period of maturation of organic matter and hydrocarbon generation in the Ordovician and Silurian source rocks was in the Late Palaeozoic (mainly Devonian-Carboniferous) and in the westernmost zone along the Teisseyre-Tornquist line at the end of the Silurian.