Przejawy mineralizacji na tle struktury metamorfiku Lądka i Śnieżnika

Stanisław Przeniosło, Hubert Sylwestrzak

Abstrakt


MINERALIZATION PHENOMENA IN THE LIGHT OF THE STRUCTURE OF LĄDEK AND ŚNIEŻNIK METAMORPHICUM

Summary
Mineralization phenomena (magnetite, fluorite, sulphide, Pb, Cu, Zn, Fe and uranium minerals) are found to occur on the Lądek and Śnieżnik Kłodzki (Eastern Sudetes) metamorphicum. The arrangement of the mineralization demonstrates that it is related to several synclinorial zones that run within the folded metamorphic formations. This fact points to a deep-seated Variscan plutonic body that, most probably, is the source of this body occurs under the synclinorial zonez at a shallower depth than under the anticlinorial ones. Thus, in the area here considered the prospections of hydrothermal deposits should be carried on in the synclinorial zones.

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