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FOSFÁT A PELOKARBONÁT Z PELITŮ PODSLEZSKÉ JEDNOTKY NA STAVBĚ SILNICE R48 U FRÝDKU-MÍSTKU, ČESKÁ REPUBLIKA
Author(s) -
Dalibor Matýsek,
Miroslav Bubík
Publication year - 2012
Publication title -
geologické výzkumy na moravě a ve slezsku v roce .../geologické výzkumy na moravě a ve slezsku v roce ...
Language(s) - English
Resource type - Journals
eISSN - 2336-4378
pISSN - 1212-6209
DOI - 10.5817/gvms2012-1-2-088
Subject(s) - fluorapatite , calcite , muscovite , siderite , geology , chlorite , quartz , mineralogy , nodule (geology) , geochemistry , sedimentary rock , apatite , paleontology
Two samples of concretions from Maastrichtian and Paleocene grey clays/claystones of the Subsilesian Unit near Frýdek-Místek two samples of concretions were studied. The sample from the Paleocene/Eocene clays of the Frýdek Formation is phosphate nodule composed of highly prevailing amount of fluorapatite, low content of quartz and small amount of chlorite, muscovite and accessories. The phosphate nodules may be in fact coprolites. The sample from the Maastrichtian Frýdek Formation is sedimentary siderite (pelosiderite) with trace content of calcite.

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