Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia

Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia

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...

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Main Authors: Wrzak-Tomić Janina, Manecki Andrzej
Format: Article
Language:English
Published: Geographical Institute "Jovan Cvijić" SASA 2004-01-01
Series:Zbornik Radova: Geografski institut "Jovan Cvijić"
Subjects:
Risavaca cave
hydrothermal
processes
karstic cycle
metasomatizam
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-7599/2004/0350-75990453027W.pdf
id doaj-31516e0cda124fdb8d39f06fb692f57f
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spelling doaj-31516e0cda124fdb8d39f06fb692f57f2020-11-25T03:43:03ZengGeographical Institute "Jovan Cvijić" SASAZbornik Radova: Geografski institut "Jovan Cvijić"0350-75991821-28082004-01-01200453274710.2298/IJGI0453027WHydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, SerbiaWrzak-Tomić JaninaManecki AndrzejIn 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.http://www.doiserbia.nb.rs/img/doi/0350-7599/2004/0350-75990453027W.pdfRisavaca cavehydrothermalprocesseskarstic cyclemetasomatizam
collection DOAJ
language English
format Article
sources DOAJ
author Wrzak-Tomić Janina
Manecki Andrzej
spellingShingle Wrzak-Tomić Janina
Manecki Andrzej
Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
Zbornik Radova: Geografski institut "Jovan Cvijić"
Risavaca cave
hydrothermal
processes
karstic cycle
metasomatizam
author_facet Wrzak-Tomić Janina
Manecki Andrzej
author_sort Wrzak-Tomić Janina
title Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
title_short Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
title_full Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
title_fullStr Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
title_full_unstemmed Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia
title_sort hydrothermal phenomena in risovaca cave and within vencac massif shumadies, serbia
publisher Geographical Institute "Jovan Cvijić" SASA
series Zbornik Radova: Geografski institut "Jovan Cvijić"
issn 0350-7599
1821-2808
publishDate 2004-01-01
description 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.
topic Risavaca cave
hydrothermal
processes
karstic cycle
metasomatizam
url http://www.doiserbia.nb.rs/img/doi/0350-7599/2004/0350-75990453027W.pdf
work_keys_str_mv AT wrzaktomicjanina hydrothermalphenomenainrisovacacaveandwithinvencacmassifshumadiesserbia
AT maneckiandrzej hydrothermalphenomenainrisovacacaveandwithinvencacmassifshumadiesserbia
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