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Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica

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2021
bitstream_1166.pdf (1.769Mb)
Authors
Kašić, Vladan
Radosavljević-Mihajlović, Ana
Radosavljević, Slobodan
Stojanović, Jovica
Mihajlović, Slavica
Vukadinović, Melina
Contributors
Stojadinović, Saša
Petrović, Dejan
Conference object (Published version)
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Abstract
Zeolites are a group of natural and artificial inorganic compounds, which have specific physicochemical properties appropriate for industrial application. These minerals make a specific group of alumosilicates within tectosilicates because of their origin, chemical compositions, structural characteristics and application. This paper presents the results of mineralogical and crystallographic examination of zeolite tuff samples from the Toponica deposit. The deposit of zeolite tuff ""Toponica"" is located in the extreme eastern part of Kosmet near Kosovska Kamenica. The immediate geological structure of the zeolite tuff deposit consists of the Lower Miocene (M) clayey sandstone, the horizon of the white zeolite tuff and the reclassified Miocene clays, clays and gravel. The basic mineral composition is the mineral clinoptilolite-Ca from the heylandite series.
Keywords:
Toponica / zeolitic tuff / clinoptilolite-heulandite group
Source:
52nd International October Conference on Mining and Metallugy IOC 2021, 2021, 181-184
Publisher:
  • Bor : University of Belgrade, Technical Faculty in Bor
Funding / projects:
  • Ministry of Education, Science and Technological Development, Republic of Serbia, Grant no. 200023 (Institute of Technology of Nuclear and Other Mineral Row Materials - ITNMS, Belgrade) (RS-200023)

ISBN: 978-86-6305-119-5

[ Google Scholar ]
URI
https://ritnms.itnms.ac.rs/handle/123456789/691
Collections
  • Radovi istraživača / Researchers’ publications
Institution/Community
Institut za tehnologiju nuklearnih i drugih mineralnih sirovina
TY  - CONF
AU  - Kašić, Vladan
AU  - Radosavljević-Mihajlović, Ana
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Mihajlović, Slavica
AU  - Vukadinović, Melina
PY  - 2021
UR  - https://ritnms.itnms.ac.rs/handle/123456789/691
AB  - Zeolites are a group of natural and artificial inorganic compounds, which have specific physicochemical properties appropriate for industrial application. These minerals make a specific group of alumosilicates within tectosilicates because of their origin, chemical compositions, structural characteristics and application. This paper presents the results of mineralogical and crystallographic examination of zeolite tuff samples from the Toponica deposit. The deposit of zeolite tuff ""Toponica"" is located in the extreme eastern part of Kosmet near Kosovska Kamenica. The immediate geological structure of the zeolite tuff deposit consists of the Lower Miocene (M) clayey sandstone, the horizon of the white zeolite tuff and the reclassified Miocene clays, clays and gravel. The basic mineral composition is the mineral clinoptilolite-Ca from the heylandite series.
PB  - Bor : University of Belgrade, Technical Faculty in Bor
C3  - 52nd International October Conference on Mining and Metallugy IOC 2021
T1  - Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica
EP  - 184
SP  - 181
ER  - 
@conference{
author = "Kašić, Vladan and Radosavljević-Mihajlović, Ana and Radosavljević, Slobodan and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2021",
abstract = "Zeolites are a group of natural and artificial inorganic compounds, which have specific physicochemical properties appropriate for industrial application. These minerals make a specific group of alumosilicates within tectosilicates because of their origin, chemical compositions, structural characteristics and application. This paper presents the results of mineralogical and crystallographic examination of zeolite tuff samples from the Toponica deposit. The deposit of zeolite tuff ""Toponica"" is located in the extreme eastern part of Kosmet near Kosovska Kamenica. The immediate geological structure of the zeolite tuff deposit consists of the Lower Miocene (M) clayey sandstone, the horizon of the white zeolite tuff and the reclassified Miocene clays, clays and gravel. The basic mineral composition is the mineral clinoptilolite-Ca from the heylandite series.",
publisher = "Bor : University of Belgrade, Technical Faculty in Bor",
journal = "52nd International October Conference on Mining and Metallugy IOC 2021",
title = "Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica",
pages = "184-181"
}
Kašić, V., Radosavljević-Mihajlović, A., Radosavljević, S., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2021). Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica. in 52nd International October Conference on Mining and Metallugy IOC 2021
Bor : University of Belgrade, Technical Faculty in Bor., 181-184.
Kašić V, Radosavljević-Mihajlović A, Radosavljević S, Stojanović J, Mihajlović S, Vukadinović M. Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica. in 52nd International October Conference on Mining and Metallugy IOC 2021. 2021;:181-184..
Kašić, Vladan, Radosavljević-Mihajlović, Ana, Radosavljević, Slobodan, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica" in 52nd International October Conference on Mining and Metallugy IOC 2021 (2021):181-184.

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