The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis
Аутори
Stojanović, JovicaPačevski, Aleksandar M.
Radosavljević-Mihajlović, Ana
Kašić, Vladan
Radosavljević, Slobodan
Остала ауторства
Mladenović, SrbaMaluckov, Čedomir
Конференцијски прилог (Објављена верзија)
Метаподаци
Приказ свих података о документуАпстракт
The Cerovo-Cementacija 2 porphyry Cu deposit, hosted by hydrothermally altered hornblende andesite,
located into the Bor Metallogenic Zone, eastern Serbia, has been investigated. In this porphyry Cu
deposit, the following mineral parageneses have been established: i) pyrite-chalcopyrite with Mo; ii)
quartz-pyrite with Au; iii) digenite-chalcocite-covellite with Au; iv) chalcedony by sulfatization and
sulphation; v) malachite-azurite-limonite. Chalcopyrite is the major Cu mineral and it is the most
abundant compared to other established Cu-sulfide minerals. By the ascending and descending
hydrothermal processes along the Zone-1 (cementation zone), chalcopyrite was commonly transformed
into secondary Cu sulfide minerals (digenite, chalcocite, anilite, covellite, etc.), while those appearances
is less represented to the Zone-2 (transitional zone).
Кључне речи:
porphyry Cu deposit / ore mineralogy / paragenetic analysis / Cerovo-Cementacija 2 / SerbiaИзвор:
The 51st International October Conference on Mining and Metallurgy, 2019, 207-211Издавач:
- Bor : University of Belgrade, Technical Faculty in Bor
Финансирање / пројекти:
- Освајање технолошких поступака добијања еколошких материјала на бази неметаличних минералних сировина (RS-MESTD-Technological Development (TD or TR)-34013)
- Синтеза, процесирање и карактеризација наноструктурних материјала за примену у области енергије, механичког инжењерства, заштите животне стредине и биомедицине (RS-MESTD-Integrated and Interdisciplinary Research (IIR or III)-45012)
- Магматизам и геодинамика Балканског полуострва од мезозоика до данас: значај за образовање металичних и неметаличних рудних лежишта (RS-MESTD-Basic Research (BR or ON)-176016)
Институција/група
Institut za tehnologiju nuklearnih i drugih mineralnih sirovinaTY - CONF AU - Stojanović, Jovica AU - Pačevski, Aleksandar M. AU - Radosavljević-Mihajlović, Ana AU - Kašić, Vladan AU - Radosavljević, Slobodan PY - 2019 UR - https://ritnms.itnms.ac.rs/handle/123456789/684 AB - The Cerovo-Cementacija 2 porphyry Cu deposit, hosted by hydrothermally altered hornblende andesite, located into the Bor Metallogenic Zone, eastern Serbia, has been investigated. In this porphyry Cu deposit, the following mineral parageneses have been established: i) pyrite-chalcopyrite with Mo; ii) quartz-pyrite with Au; iii) digenite-chalcocite-covellite with Au; iv) chalcedony by sulfatization and sulphation; v) malachite-azurite-limonite. Chalcopyrite is the major Cu mineral and it is the most abundant compared to other established Cu-sulfide minerals. By the ascending and descending hydrothermal processes along the Zone-1 (cementation zone), chalcopyrite was commonly transformed into secondary Cu sulfide minerals (digenite, chalcocite, anilite, covellite, etc.), while those appearances is less represented to the Zone-2 (transitional zone). PB - Bor : University of Belgrade, Technical Faculty in Bor C3 - The 51st International October Conference on Mining and Metallurgy T1 - The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis EP - 211 SP - 207 ER -
@conference{ author = "Stojanović, Jovica and Pačevski, Aleksandar M. and Radosavljević-Mihajlović, Ana and Kašić, Vladan and Radosavljević, Slobodan", year = "2019", abstract = "The Cerovo-Cementacija 2 porphyry Cu deposit, hosted by hydrothermally altered hornblende andesite, located into the Bor Metallogenic Zone, eastern Serbia, has been investigated. In this porphyry Cu deposit, the following mineral parageneses have been established: i) pyrite-chalcopyrite with Mo; ii) quartz-pyrite with Au; iii) digenite-chalcocite-covellite with Au; iv) chalcedony by sulfatization and sulphation; v) malachite-azurite-limonite. Chalcopyrite is the major Cu mineral and it is the most abundant compared to other established Cu-sulfide minerals. By the ascending and descending hydrothermal processes along the Zone-1 (cementation zone), chalcopyrite was commonly transformed into secondary Cu sulfide minerals (digenite, chalcocite, anilite, covellite, etc.), while those appearances is less represented to the Zone-2 (transitional zone).", publisher = "Bor : University of Belgrade, Technical Faculty in Bor", journal = "The 51st International October Conference on Mining and Metallurgy", title = "The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis", pages = "211-207" }
Stojanović, J., Pačevski, A. M., Radosavljević-Mihajlović, A., Kašić, V.,& Radosavljević, S.. (2019). The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis. in The 51st International October Conference on Mining and Metallurgy Bor : University of Belgrade, Technical Faculty in Bor., 207-211.
Stojanović J, Pačevski AM, Radosavljević-Mihajlović A, Kašić V, Radosavljević S. The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis. in The 51st International October Conference on Mining and Metallurgy. 2019;:207-211..
Stojanović, Jovica, Pačevski, Aleksandar M., Radosavljević-Mihajlović, Ana, Kašić, Vladan, Radosavljević, Slobodan, "The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis" in The 51st International October Conference on Mining and Metallurgy (2019):207-211.