Products and timing of diagenetic processes in Upper Rotliegend sandstones from Bebertal (North German Basin, Parchim Formation, Flechtingen High, Germany)
- 31 January 2012
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 149 (5) , 827-840
Abstract
Aeolian-fluvial Upper Rotliegend sandstones from Bebertal outcrops (Flechtingen High, North Germany) are an analogue for deeply buried Permian gas reservoir sandstones of the North German Basin (NGB). We present a paragenetic sequence as well as thermochronological constraints to reconstruct the diagenetic evolution and to identify periods of enhanced mesodiagenetic fluid–rock reactions in sandstones from the southern flank of the NGB. Bebertal sandstones show comparatively high concentrations of mesodiagenetically formed K-feldspar but low concentrations of illite cements. Illite-rich grain rims were found to occur preferentially directly below sedimentary bounding surfaces, i.e. aeolian superimposition surfaces, and indicate the lowest intergranular volume. Illite grain rims also indicate sandstone sections with low quartz and feldspar cement concentrations but high loss of intergranular volume due to compaction.40Ar–39Ar age determination of pronounced K-feldspar grain overgrowths and replacements of detrital grains indicates two generations: an early (Triassic) and a late (Jurassic) generation. The latter age range is similar to published diagenetic illite ages from buried Rotliegend reservoir sandstones. The first generation suggests an early intense mesodiagenetic fluid flow with remarkably high K+activity synchronous with fast burial of proximal, initial graben sediments on the southern flank of the NGB. Accordingly, zircon fission-track data indicate that the strata already reached the zircon partial annealing zone of approximately 200°C during early mesodiagenesis. Zircon (U–Th)/He ages (92 ± 12 Ma) as well as apatite fission-track ages (~ 71–75 Ma) indicate the termination of mesodiagenetic processes, caused by rapid exhumation of the Flechtingen High during Late Cretaceous basin inversion.Keywords
This publication has 52 references indexed in Scilit:
- Provenance of Cretaceous clastics in the Subhercynian Basin: constraints to exhumation of the Harz Mountains and timing of inversion tectonics in Central EuropeInternational Journal of Earth Sciences, 2007
- Dynamics of sedimentary basins: the example of the Central European Basin systemInternational Journal of Earth Sciences, 2005
- Late Permian non-marine–marine transitional profiles in the central Southern Permian Basin, northern GermanyInternational Journal of Earth Sciences, 2005
- The southern margin of the East European Craton: new results from seismic sounding and potential fields between the North Sea and PolandTectonophysics, 2002
- An integrated study of the NE German BasinTectonophysics, 1999
- Controls on Clay Mineral Distribution and Chemistry in the Early Permian Rotliegend of GermanyClay Minerals, 1993
- Experimental Determination of the Rates of Precipitation of Authigenic Illite and Kaolinite in the Presence of Aqueous Oxalate and Comparison to the K/Ar Ages of Authigenic Illite in Reservoir SandstonesClays and Clay Minerals, 1993
- Lower permian rotliegend sandstones, southern north sea: a case study of sandstone diagenesis in evaporite-associated sequencesSedimentary Geology, 1992
- A new look at statistics in fission-track datingNuclear Tracks, 1981
- Fission-track dating methods: What are the real alternatives?Nuclear Tracks, 1981