Hydrocarbon potential of the Zechstein Main Dolomite in the western part of the Wielkopolska platform, SW Poland: New sedimentological and geochemical data

Kosakowski, Paweł; Krajewski, Marcin

doi:10.1016/j.marpetgeo.2013.10.002

Cited by 18 publications

(30 citation statements)

References 37 publications

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“…The results enabled us to identify main components and textures using the standard criteria and the carbonate classification (Dunham, 1962;Embry and Klovan, 1972). Microfacies recognized on the Gorz ow Platform were related to the newly developed standard classification of the microfacies association and facies in the Polish part of the Southern Permian Basin (Kosakowski and Krajewski, 2014). The application of this methodology allows on a broader regional comparison of the areas belonging to the Zechstein petroleum system.…”

Section: Samples and Methodsmentioning

confidence: 99%

“…Kosakowski and Krajewski, 2014), which represent facies typical of paleogeographic zones of the Main Dolomite in the SPB. The 15 types were selected (Types IeXV).…”

Section: Facies Sequence Stratigraphy and Depositional Model E Resulmentioning

confidence: 99%

“…The contemporary state of knowledge on the subject is poor and not sufficient. Both, previously conducted studies (Kosakowski and Krajewski, 2014) and new unpublished data from Gorzow Platform can contribute to a better understanding of the petroleum system in the analyzed area.…”

Section: Introductionmentioning

confidence: 99%

“…The Main Dolomite sediments are simultaneously petroleum source rocks and reservoirs due to perfect sealing from over-and underlying anhydrite and rock salt strata Mikołajewski, 2009, 2011;Kosakowski and Krajewski, 2014). Therefore, determination of qualitative and quantitative are aimed at comprehensive development of facies and microfacies of the Ca2 in the Grot ow Platform, and comparison with results of geochemical analyses.…”

Section: Introductionmentioning

confidence: 99%

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Hydrocarbon potential of the Zechstein Main Dolomite (Upper Permian) in western Poland: Relation to organic matter and facies characteristics

Kosakowski

Krajewski

2015

Marine and Petroleum Geology

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Section: Samples and Methodsmentioning

confidence: 99%

“…Kosakowski and Krajewski, 2014), which represent facies typical of paleogeographic zones of the Main Dolomite in the SPB. The 15 types were selected (Types IeXV).…”

Section: Facies Sequence Stratigraphy and Depositional Model E Resulmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Hydrocarbon potential of the Zechstein Main Dolomite (Upper Permian) in western Poland: Relation to organic matter and facies characteristics

Kosakowski

Krajewski

2015

Marine and Petroleum Geology

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“…In contrast, Fishman et al (2013) recognized nanoporosity in high maturity (~1.2% VRo) migrated bitumen from Eagle Ford Shale core samples equivalent to the post-oil solid bitumen terminology used here. Kosakowski and Krajewski (2014, their figure 11E) recognized a post-oil solid bitumen network in carbonates in Poland.…”

Section: Accepted Manuscriptmentioning

confidence: 99%

Post-oil solid bitumen network in the Woodford Shale, USA — A potential primary migration pathway

Cardott

Landis²,

Curtis

2015

International Journal of Coal Geology

194

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Crescentiella-microbial-cement microframeworks in the Upper Jurassic reefs of the Crimean Peninsula

Krajewski

Schlagintweit²

2018

Facies

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In the Upper Jurassic reef successions of the Crimean Peninsula (Sudak and Jalta areas), the microencruster Crescentiella morronensis (Crescenti), microbialites, and multiple generations of cements, form microframeworks. They were observed in two stages of the carbonate platform evolution, in the Middle-Upper Oxfordian, and in the Upper Kimmeridgian-Tithonian. Generally, in both stages, the features of the microframeworks are similar and consist of densely packed Crescentiella associated with microbialites and branched colonies of the sclerosponge Neuropora lusitanica Termier. The difference between the occurrences of the two stages is the variable amount of nubecularid foraminifera and enigmatic tube-shaped structures forming the central cavities of Crescentiella. The Crescentiella-microbial-cement microframeworks formed under phreatic conditions in the upper slope and seaward marginal depositional settings where intensive synsedimentary cementation took place. They formed in the initial stages of long cycles of restoration and blooming of the reefs. The late Jurassic examples resemble the Permian algae-microbial-cement reefs as well as the Triassic Tubiphytes and cement crust-dominated reefs. Concurrently, all these examples formed a transitional facies zone between typical slope facies to shallow subtidal platform margin facies characterized by high taxonomic diversity of calcified sponges, corals, and microencrusters forming the principal part of the reefs.

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Hydrocarbon potential of the Zechstein Main Dolomite in the western part of the Wielkopolska platform, SW Poland: New sedimentological and geochemical data

Cited by 18 publications

References 37 publications

Hydrocarbon potential of the Zechstein Main Dolomite (Upper Permian) in western Poland: Relation to organic matter and facies characteristics

Hydrocarbon potential of the Zechstein Main Dolomite (Upper Permian) in western Poland: Relation to organic matter and facies characteristics

Post-oil solid bitumen network in the Woodford Shale, USA — A potential primary migration pathway

Crescentiella-microbial-cement microframeworks in the Upper Jurassic reefs of the Crimean Peninsula

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