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This article focuses on a newly identified set of crevasse splays in the lignite-bearing Miocene of Poland. The sand bodies studied are situated within the First Mid-Polish Lignite Seam (MPLS-1) in the Tomisławice opencast mine, located near Konin in central Poland. The sand bodies form an alluvial complex of four superposed crevasse splays, separated by lignite layers, 0.1–0.8 m thick. They are considered to be overbank lateral splays, emplaced laterally by a fluvial channel, rather than its terminal splays. Their combined thickness reaches ~5 m, their length is <0.6 km and width <0.4 km, and their total area is ~0.1 km2. Nearly half of the sediments examined are subaerial deposits, while the rest are typical of crevasse-splay microdeltas, accumulated in a floodplain subaqueous environment. The sand bodies with local clay lenses are both underlain and overlain by, as well as interbedded with a range of lignite lithotypes, representing various sub-environments of a mid-Miocene mire (backswamp) realm. The estimated time span for the formation of the entire crevasse-splay complex, recording four short-term floods, is at least 48 kyr. The crevasse-splay complex is one of the best developed in lignite/coal successions worldwide. However, it poses a major technical obstacle to mining activity in the Konin Lignite Mine.
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Bibliogr.126 poz., fot., rys., tab., wykr.
Twórcy
autor
- Institute of Geology, Adam Mickiewicz University, Krygowskiego 12, 61-680 Poznań, Poland
autor
- Konin Lignite Mine, 600-lecia 9, 62-540 Kleczew, Poland
autor
- Institute of Geology, Adam Mickiewicz University, Krygowskiego 12, 61-680 Poznań, Poland
autor
- Konin Lignite Mine, 600-lecia 9, 62-540 Kleczew, Poland
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