Inside-out solution of carbonate clasts - an analogue model for hypogene karstification (CROSBI ID 593458)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa
Podaci o odgovornosti
Marjanac, Tihomir ; Adžić, Ivana ; Blažić, Luka ; Marjanac, Ljerka
engleski
Inside-out solution of carbonate clasts - an analogue model for hypogene karstification
Voids in Miocene (Badenian) limestone of the Medvednica Mt. in Croatia, locally known as "Litavac", were recognized as solution casts of Upper Triassic dolomite fragments. These voids are actually micro-caverns since they occur inside partly dissolved dolomite clasts. Identical micro-caverns are also recognized in limestone cobbles of Jurassic age in Pleistocene coarse-grained deltaic conglomerates of Seline in Northern Dalmatia. Partial solution of bituminous carbonate debris represents a possible small-scale analogue to formation of large hypogene caverns of Dinaric Alps where formation waters with dissolved H2S (sulfuric acid) dissolved fractured bituminous host rocks.
karstification; hypogene karst; carbonate solution
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Podaci o prilogu
46-46.
2012.
objavljeno
Podaci o matičnoj publikaciji
Abstracts
Mihevc, Andrej ; Gabrovšek, Franci
Postojna: Znanstvenoraziskovalni center SAZU, Inštitut za raziskovanje krasa ZRC SAZU = Karst Research Institute at ZRC SAZU
Podaci o skupu
20. International Karstological School "Classical Karst" : Karst Forms and Processes
poster
18.06.2012-23.06.2012
Postojna, Slovenija