Deposits of zeolite tuffs, rich in minerals of the heylandite-clinoptilolite series, in Serbia are
spatially and genetically related to volcanogenic-sedimentary series of sedimentary basins and
were formed as a product of devitrification of volcanic glass. Zeolite minerals in sedimentary
rocks of Neogene age are found in association with volcanic and volcaniclastic rocks. The
lacustrine or marine environment had a great influence on the diagenesis of sediments and the
formation of clinoptilolite at the expense of volcanic glass. In this paper, a preliminary model of
the formation of zeolite deposits in the Tertiary basins of Serbia is presented, through the
processing of all elements of the genetic model.
Keywords:
zeolitic tuff / genetic model / clinoptilolite-heulandite group / Serbia deposit
Source:
53nd International October Conference on Mining and Metallurgy IOC 2022, 2022, 67-70
TY - CONF
AU - Kašić, Vladan
AU - Radosavljević, Slobodan
AU - Simić, Vladimir
AU - Radosavljević-Mihajlović, Ana
AU - Stojanović, Jovica
AU - Mihajlović, Slavica
AU - Vukadinović, Melina
PY - 2022
UR - https://ritnms.itnms.ac.rs/handle/123456789/687
AB - Deposits of zeolite tuffs, rich in minerals of the heylandite-clinoptilolite series, in Serbia are
spatially and genetically related to volcanogenic-sedimentary series of sedimentary basins and
were formed as a product of devitrification of volcanic glass. Zeolite minerals in sedimentary
rocks of Neogene age are found in association with volcanic and volcaniclastic rocks. The
lacustrine or marine environment had a great influence on the diagenesis of sediments and the
formation of clinoptilolite at the expense of volcanic glass. In this paper, a preliminary model of
the formation of zeolite deposits in the Tertiary basins of Serbia is presented, through the
processing of all elements of the genetic model.
PB - Bor : Mining and Metallurgy Institute Bor
C3 - 53nd International October Conference on Mining and Metallurgy IOC 2022
T1 - Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia
EP - 70
SP - 67
ER -
@conference{
author = "Kašić, Vladan and Radosavljević, Slobodan and Simić, Vladimir and Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2022",
abstract = "Deposits of zeolite tuffs, rich in minerals of the heylandite-clinoptilolite series, in Serbia are
spatially and genetically related to volcanogenic-sedimentary series of sedimentary basins and
were formed as a product of devitrification of volcanic glass. Zeolite minerals in sedimentary
rocks of Neogene age are found in association with volcanic and volcaniclastic rocks. The
lacustrine or marine environment had a great influence on the diagenesis of sediments and the
formation of clinoptilolite at the expense of volcanic glass. In this paper, a preliminary model of
the formation of zeolite deposits in the Tertiary basins of Serbia is presented, through the
processing of all elements of the genetic model.",
publisher = "Bor : Mining and Metallurgy Institute Bor",
journal = "53nd International October Conference on Mining and Metallurgy IOC 2022",
title = "Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia",
pages = "70-67"
}
Kašić, V., Radosavljević, S., Simić, V., Radosavljević-Mihajlović, A., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2022). Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia. in 53nd International October Conference on Mining and Metallurgy IOC 2022
Bor : Mining and Metallurgy Institute Bor., 67-70.
Kašić V, Radosavljević S, Simić V, Radosavljević-Mihajlović A, Stojanović J, Mihajlović S, Vukadinović M. Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia. in 53nd International October Conference on Mining and Metallurgy IOC 2022. 2022;:67-70..
Kašić, Vladan, Radosavljević, Slobodan, Simić, Vladimir, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia" in 53nd International October Conference on Mining and Metallurgy IOC 2022 (2022):67-70.
