The impact of diagenesis on the reservoir properties of Mesozoic sedimentary rocks of the Łódź and Miechów troughs, central Poland
DOI:
https://doi.org/10.7306/gq.1801Keywords:
diagenesis, reservoir properties, Mesozoic sedimentary rocks, Łódź and Miechów troughsAbstract
Mesozoic siliciclastic and carbonate strata, analysed in 28 boreholes located in the Łódź and Miechów troughs, Poland, comprise Triassic and Jurassic rocks accumulated under terrestrial and marine conditions, and Cretaceous deposits of marine origin. Siliciclastic rocks (sandstones, siltstones, mudstones and claystones, with subordinate conglomerates) are the main lithofacies in the Lower and Upper Triassic, Lower and Middle Jurassic, and in the Lower Cretaceous. Carbonate rocks dominate in the Middle Triassic and Upper Jurassic. The Upper Cretaceous succession is represented by siliceous-carbonate deposits. These sedimentary rocks were studied in terms of sedimentary basin analysis and in particular as regards their reservoir characteristics, with detailed petrographic and porosity studies of these rocks and special emphasis on the sandstones and limestones. The focus was on the effects of diagenetic processes and their influence on reservoir properties. The most important diagenetic processes that affected the reservoir properties of the rocks were compaction, cementation and dissolution, and also replacement in carbonate rocks. Compaction and cementation have reduced the porosity of the sandstones by an average of ~44% and 29%, respectively. The effects of dissolution, mainly of feldspar grains and bioclasts, contributed to the development of secondary porosity in the rocks. Replacement processes – dolomitization of limestones – also increased the porosity of the rocks. Sandstones with good reservoir properties (porosity >15%, permeability >100 mD) are found in the Lower Triassic (Buntsandstein), Lower Jurassic and Lower Cretaceous. Among the carbonates, the Middle Triassic (Muschelkalk) deposits show the best reservoir properties, but most of the porous (>10%) carbonate and carbonate-marly rocks are impermeable. The Miechów Trough, by comparison with the Łódź Trough, includes better reservoir properties.Downloads
Published
2025-09-09
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).

