Slump folds within mid-Miocene crevasse-splay deposits: a unique example from the Tomisławice lignite opencast mine in central Poland
Sign Up to like & getrecommendations! Published in 2020 at "Geological Quarterly"
DOI: 10.7306/gq.1545
Abstract: Non-tectonic, soft-sediment deformation structures occur in mid-Miocene crevasse-splay deposits exposed in the Tomislawice lignite opencast mine in central Poland. The crevasse-splay cross-stratified siliciclastic deposits are underlain by continuously folded and relatively thick lignite beds, and… read more here.
Keywords: miocene crevasse; lignite; crevasse; mid miocene ... See more keywords