relations of the hydrothermal mineralisation to the structures in the rudòany ore field

Clicks: 65
ID: 143066
1997
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Abstract
In the area of the Rudòany ore field (NE part of Spišsko – gemerské Ore Mts, Slovakia) the hydrothermal vein mineralisation is connected with cleavage planes, faults and with host - rocks boundaries. As a rule vein-type mineral associations occupy structures of the „S“ cleavage systems, which were generated during VD1 deformation stage of the hercynian (variscan) orogeny and also during AD1 to AD3 deformation stages of the alpine orogenetical cycle. Analysis of mineralised tectonical structures is based on genetical and successive conditions of the mineralised associations in the relation to the structural-tectonical domains.
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tibor1997actarelations Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Sasvári Tibor
Journal comparative biochemistry and physiology toxicology & pharmacology : cbp
Year 1997
DOI
DOI not found
URL
http://actamont.tuke.sk/pdf/1997/n4/3sasvari.pdf
Keywords Keywords not found

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