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GYPSUM DEPOSITS IN THE REPUBLIC OF CROATIA

Anto Gabrić
Boris Šinkovec
Krešimir Sakač
Gordan Kuljak

Sažetak

The occurences and deposits of gypsum can be found in big karst poljes (Sinjsko, Vrličko, Petrovo, Kosovo and Kninsko) as well as in tectonnically predestined river valleys of Zrmanja, Butišnica and Una. There also appear spatially localized occurences on the island of Vis and in the vicinity of Samobor.
Evaporites (gypsum and anhydrite) with adjoining overlying clastic rocks (red sandstones, siltites and pelites), carbonate rocks (dolomites and limestones) and porous carbonate breccias (Rauhwackes) were deposited during the period of Upper Permian. The recent position of the Upper Permian beds is a result of complex tectonic, particularly neotectonic, movements and diapiric displacements. Evaporites were deposited in marginal areas of the epicontinental marine basin, in a period of favourable conditions for the sabkha and playa sedimentation due to the continuous shoreline progradation. The Upper Permian age of these sediments in Dalmatio is proved by the characteristic mineral paragenesis and palinological determinations in elastics rocks, as well as by isotope analyses of sulphure in gypsum.
Gypsum is a significant ore mineral resource in building, cement production, as well as in a number of tehnological processes used in chemical industry and elsewhere. According to the recent investigations gypsum is predestined to serve as an ore mineral resource of significant perspectives.

Ključne riječi

gypsum; anhydrite; evaporites; clastic rocks; carbonate rocks; igneous rocks; rauhwackes; Upper Permian; diapirism; tectogenesis; hydratation; Dalmatia; Lika; Samobor Mountains

Hrčak ID:

7383

URI

https://hrcak.srce.hr/7383

Datum izdavanja:

4.12.2002.

Podaci na drugim jezicima: hrvatski

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