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- W2565037458 abstract "The deposits of the Gresten Formation (Midle Jurassic) obtainedfrom deep wells in the territory of southern Moravia (CzechRepublic) have been newly examined with the aim to betterdescribe their provenance and depositional environment.Deposition within a relatively broad flood plain withfluvial/distributive channels, crevasse channels, crevassessplays and coal-swaps have been recognised in the majority ofwell cores. Basinal/open marine deposits have been less common.The heavy mineral association is quite stable, with significantdominance of garnet and commonly also with high content ofzircon. The mineralogical spectra of garnet types were broadwith strong dominance of almandines. The rutiles were mostlyderived from metapelites and additionally also from metamaficrocks and pegmatites. The results point to mixed sources fromboth intensively weathered crystalline rocks of the easternmargin of the Bohemian Massif (primary source) and the oldersedimentary rocks - especially from the Moravo-SilesianPaleozoic deposits (recycled source)." @default.
- W2565037458 created "2017-01-06" @default.
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- W2565037458 date "2016-01-01" @default.
- W2565037458 modified "2023-09-27" @default.
- W2565037458 title "Depositional environment and provenance of the Gresten Formation (Middle Jurassic) on the southeastern slopes of the Bohemian Massif (Czech Republic, subsurface data)" @default.
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- W2565037458 doi "https://doi.org/10.17738/ajes.2016.0020" @default.
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