Magmatski epidot Željina (Centralna Srbija)

Igneus epidote of Željin (Central Serbia)

Authors

  • Milenko Vukov University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
  • Istvan Forizs Laboratory for Geochemical Research of the Hungarian Academy of Sciences, 1112, Budapest, Budaorsi zt 45, Hungary.
  • Mihovil Logar University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.

Keywords:

Igneous epidote, metamorphic epidote, chemistry, physical and chemical conditions

Abstract

This paper discusses the results of a chemical and mineralogical (DTA) study of epidote from the granitoid pluton of Željin. The available experimental and empurical data are analysed to study the possible fomiation of a Željin epidote generation (mEp) under igneous conditions. The established (and published) chemical and mineralogical properties of coexistent minerals: Ep, Bt, and Hbl, and respective chemical attributes of rocks, are used in the consideration.

 

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Published

1997-12-20

Issue

Vol. 61 No. 2 (1997): Geološki anali Balkanskoga poluostrva

Section

Original Scientific Paper

How to Cite

“Magmatski epidot Željina (Centralna Srbija): Igneus epidote of Željin (Central Serbia)” (1997) Geološki anali Balkanskoga poluostrva, 61(2), pp. 401–417. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/385 (Accessed: 4 November 2026).