hydrothermal phenomena in risovaca cave and within vencac massif shumadies, serbia

hydrothermal phenomena in risovaca cave and within vencac massif shumadies, serbia

;Wrzak-Tomić Janina;Manecki Andrzej
advanced materials research 2004 Vol. 2004 pp. 27-47
160
janina2004zbornikhydrothermal

Abstract

In the Risovaca cave are found, for the karst, atypical alteration in the limestones structure. Also, morphogenesis of the object can not be logically interpret. Those differences are result of hydrothermal process in initial phase of karstic cycle. And then activity of hot water and hot emanations brought up to the metasomatism and destruction of rock, enormous excrete of ornaments and later, ceiling collapse and fill up of cave room.

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ID: 164196
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