An Organic Geochemical, Study to Compare Jurassic Black Shale-hosted Manganese Carbonate Deposits: Urkut, Hungary, and Branisko Mountains, East Slovakia

Exploration & Mining Geology, Vol. 1, No. 1, 1992
MARTA POLGARI, Laboratory for Geochemical Research, Hungarian Academy of Sciences, Budapes, and BOHUMIL MOLAK and EVA SUROVA, Geologicky ustav Dionyza Shira, Mlynska dolina 1, Bratislova
Abstract The Urkut rhodochrosite deposit and Branisko Mn showings (rancieite, manganiferous calcite), located in Lower Jurassic marine sedimentary rocks with black shale, were studied by organic-geochernical methods. Both depositional localities were affected by the Lower Jurassic Toarcian anoxic event. Urkiit shales are rich in organic matter (av. 2.94 wt^o total organic carbon), the composition of which indicates derivation mainly from marine sources, with some terrigenous component. The shales matured in a bacterialry active environment under reducing conditions of diagenesis-catagenesis. Branisko shales (—0.2 wt% TOQ with lenses of Mn oxide ore were weakly metamorphosed and their organic matter thermally degraded. The model for Mn carbonate ore formation envisages reaction of Mn derived from sediments, with carbonate generated by a bacterially mediated process of decomposition of organic matter that also involved Mn reduction. »
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