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This is a Fe-concretion (about 2 cm in diameter) of possible sedimentary origin (Carpathian Flysch; reflected light microscopy). I suppose the dark grains are could be quartz, subsequently...
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The material is probably Cretaceous chert (or jasper? - in the picture on the right there are probably intrusions of agate) from the contact with submarine volcanic rocks from the Flysch Zone of...
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