engleski

The Succession of Metamorphic Parageneses in Mineral Assemblage from Marble - Creek Zorovac (Moslavačka gora, Northern Croatia)

Mineral assemblage in marble from Zorovac Creek (Moslavačka Gora) is represented by 24 different minerals (not final list) which could not form in one single metamorphic event. During complex evolution of crystalline terrain of Moslavačka gora, parageneses are developed depending on present metamorphic conditions and successively followed each other. Due to slow reaction rate there are relics of older parageneses which together with numerous metamorphic reactions in the system (SiO2-TiO2-Al2O3-FeO-MnO-CaO-MgO-Na2O-K2O-CO2-H2O-HF) contribute to the diversity of mineral species in assemblage.

marble; metamorphic reactions; paragenesis; assemblage; crystalline basement; Pannonian Basin; Moslavačka Gora; South Tisia

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