Facies, Paleogeography, and Sedimentary History of the Southern Permian Basin in Europe

Kiersnowski, Hubert; Paul, Josef; Peryt, Tadeusz Marek; Smith, Douglas R.

doi:10.1007/978-3-642-78590-0_7

Cited by 55 publications

(41 citation statements)

References 26 publications

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“…One of these ridges, the Wolsztyn Palaeo-Ridge, part of the Vari scan externides, sep a rated two Rotliegend sed i men tary bas ins (Zielona Góra Ba sin and the Vari scan Fore land) where playa lake, ae olian and wadi de pos its up to 1000 m thick ac cu mu lated dur ing Mid dle and the ear li est Late Perm ian times. Those silici clastic rocks are absent from the Wolsztyn Ridge or are re placed by coeval vol ca nic rocks (Kiersnowski et al, 1995(Kiersnowski et al, , 2010.…”

Section: Geological Settingmentioning

confidence: 99%

Polyphase dolomitization of the Wuchiapingian Zechstein Limestone (Ca1) isolated reefs (Wolsztyn Palaeo-Ridge, Fore-Sudetic Monocline, SW Poland)

Jasionowski

Peryt

Durakiewicz

2014

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Section: Geological Settingmentioning

confidence: 99%

Polyphase dolomitization of the Wuchiapingian Zechstein Limestone (Ca1) isolated reefs (Wolsztyn Palaeo-Ridge, Fore-Sudetic Monocline, SW Poland)

Jasionowski

Peryt

Durakiewicz

2014

Self Cite

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“…North Greenland Gruszczynski et al, 1989;Stemmerik and Worsley, 1989;Ezaki et al, 1994;Stemmerik, 1997Stemmerik, , 2000 11. BjÖrnÖya Kiersnowski et al, 1995;Smith, 1981a,b cold water during the Guadalupian (Beauchamp, 1994;Beauchamp and Desrochers, 1997). Evidence for a Guadalupian landward expansion of silica factories and a coeval contraction of carbonate factories can be found all along the western margin of North America (Fig.…”

Section: Expansion Of Pce: Guadalupianmentioning

confidence: 99%

Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohaline circulation

Beauchamp

Baud

2002

Palaeogeography, Palaeoclimatology, Palaeoecology

266

132

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The Permian Chert Event (PCE) was a 30 Ma long episode of unusual chert accumulation along the northwest margin of Pangea, and possibly worldwide. The onset of the PCE occurred at about the Sakmarian^Artinskian boundary in the Sverdrup Basin, Canadian Arctic, where it coincides with a maximum flooding event, the ending of high-frequency/high-amplitude shelf cyclicity, the onset of massive biogenic chert deposition in deep-water distal areas, and a long-term shift from warm-to cool-water carbonate sedimentation in shallow-water proximal areas. A similar and coeval shift is observed from the Barents Sea to the northwestern USA. A landward and southward expansion of silica factories occurred during the Middle and Late Permian at which time warm-water carbonate producers disappeared completely from the northwest margin of Pangea. Biotically impoverished and increasingly narrow cold-water carbonate factories (characterised by non-cemented bioclasts of sponges, bryozoans, echinoderms and brachiopods) were then progressively replaced by silica factories. By Late Permian time, little carbonate sediments accumulated in the Barents Sea and in the Sverdrup Basin, where the deep-to shallow-water sedimentary spectrum was occupied by siliceous sponge spicules. By that time, biogenic silica sedimentation was common throughout the world. Silica factories collapsed in the Late Permian, abruptly bringing the PCE to an end. In northwest Pangea, the end-Permian collapse of the PCE was associated with a major transgression and with a return to much warmer oceanic and continental climatic conditions. Chert deposition resumed in the distal oceanic areas during the early Middle Triassic (Anisian) after a 8^10 Ma interruption (Early Triassic Chert Gap). The conditions necessary for the onset, expansion and zenith of the PCE were provided by the thermohaline circulation of nutrient-rich cold waters along the northwestern and western margin of Pangea, and possibly throughout the world oceans. These conditions provided an efficient transportation mechanism that constantly replenished the supply of silica in the area, created a nutrient-and oxygen-rich environment favouring siliceous biogenic productivity, established cold sea-floor conditions, hindering silica dissolution, while increasing calcium carbonate solubility, and provided conditions adverse to organic and inorganic carbonate production. The northwest margin of Pangea was, for nearly 30 Ma, bathed by cold waters presumably derived from the seasonal melting of northern sea ice, the assumed engine for thermohaline circulation.This process started near the Sakmarian^Artinskian boundary, intensified throughout Middle and Late Permian time and ceased suddenly in latest Permian time. It led to oceanic conditions much colder than normally expected from the palaeolatitudes, and the influence of cold northerly-derived water was felt as far south southern Nevada. The demise of silica factories was caused by the rapid breakdown of these conditions and the establishment of a much warm...

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“…The interval region was situated at that time on the southern flank of the Polish Basin, known as the Mid-Polish Trough (MPT), which in turn was part of the Permian-Mesozoic system of epicontinental basins of Western and Central Europe, overlapping to a great extent the area of the Southern Permian Basin (SPB). The Polish Basin was the eastern part of the SPB (Ziegler, 1990;Kiersnowski et al, 1995;Krzywiec, 2006;Jarosiński et al, 2009;Gast et al, 2010;Pharaoh et al, 2010). Its development resulted from longterm thermal subsidence, which started in the Permian and lasted until the Late Cretaceous.…”

Section: Geological Settingsmentioning

confidence: 99%

Structural and Parametric Models of the Załęcze and Żuchlów Gas Field Region, Fore-Sudetic Monocline, Poland – An Example of a General Static Modeling Workflow in Mature Petroleum Areas for CCS, EGR or EOR Purposes

Papiernik

Doligez

Klimkowski

2015

Oil Gas Sci. Technol. – Rev. IFP Energies nouvelles

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-Załęcze and Żuchlów are strongly depleted natural gas fields in aeolian sandstones of the Rotliegend, located in the central part of the Fore-Sudetic Monocline. A set of three static 3D models was generated to check the possibility of CO 2 injection for Enhanced Gas Recovery (EGR) and to check the safety of storage by means of geomechanical modeling: one regional model (ZZA) and two local models -the first for Załęcze (ZA) gas field and the second for Żuchlów (ZU) gas field. The regional model is composed of 12 stratigraphic complexes (zones) from the base of the Rotliegend to the ground surface. The local models comprise only the three lowermost complexes: fluvial deposits of the Rotliegend, aeolian sandstones of the Rotliegend (Reservoir I) and basal Zechstein limestone, Ca1. The key elements of the modeling procedure include: Quality Control (QC) of the data, interpretation of missing parameters necessary for static modeling and their integration within a geomodel. The processing workflow was elaborated to produce convergent regional and local models. The regional static model is a framework for a regional geomechanical model. The local models are the basis for dynamic simulations and local geomechanical modeling. The presented workflow could be used with some changes for geomodeling of many mature gas and oil fields.Résumé -Modèles structurels et paramétriques de la région des gisements de gaz de Załęcze et Żuchlów, Région monoclinale des Sudètes, Pologne -un exemple du déroulement d'une modélisation statique générale dans des zones de pétrole matures dans un but de CCS, EGR ou d'EOR -Załęcze et Żuchlów sont des gisements de gaz naturel largement épuisés dans les sables éoliens du Rotliegend, situés au centre de la structure monoclinale des Sudètes. Un ensemble de trois modèles en 3D statiques a été généré, afin de vérifier la possibilité d'injecter du CO 2 pour améliorer la récupération du gaz et de vérifier la sécurité de stockage au moyen d'une modélisation géomécanique : un modèle régional (ZZA) et deux modèles locaux -le premier pour le gisement de gaz de Załęcze (ZA) et le second pour le gisement de gaz de Żuchlów (ZU). Le modèle régional est

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Facies, Paleogeography, and Sedimentary History of the Southern Permian Basin in Europe

Cited by 55 publications

References 26 publications

Polyphase dolomitization of the Wuchiapingian Zechstein Limestone (Ca1) isolated reefs (Wolsztyn Palaeo-Ridge, Fore-Sudetic Monocline, SW Poland)

Polyphase dolomitization of the Wuchiapingian Zechstein Limestone (Ca1) isolated reefs (Wolsztyn Palaeo-Ridge, Fore-Sudetic Monocline, SW Poland)

Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohaline circulation

Structural and Parametric Models of the Załęcze and Żuchlów Gas Field Region, Fore-Sudetic Monocline, Poland – An Example of a General Static Modeling Workflow in Mature Petroleum Areas for CCS, EGR or EOR Purposes

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