Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica
Аутори
Kašić, VladanRadosavljević-Mihajlović, Ana
Radosavljević, Slobodan
Stojanović, Jovica
Mihajlović, Slavica
Vukadinović, Melina
Остала ауторства
Stojadinović, SašaPetrović, Dejan
Конференцијски прилог (Објављена верзија)
Метаподаци
Приказ свих података о документуАпстракт
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.
Кључне речи:
Toponica / zeolitic tuff / clinoptilolite-heulandite groupИзвор:
52nd International October Conference on Mining and Metallugy IOC 2021, 2021, 181-184Издавач:
- Bor : University of Belgrade, Technical Faculty in Bor
Финансирање / пројекти:
- Министарство науке, технолошког развоја и иновација Републике Србије, институционално финансирање - 200023 (Институт за технологију нуклеарних и других минералних сировина - ИТНМС, Београд) (RS-MESTD-inst-2020-200023)
Институција/група
Institut za tehnologiju nuklearnih i drugih mineralnih sirovinaTY - 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.