Претрага
523 items
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Groundwater gravitational circulation of Karst Veliko Vrelo and Malo Vrelo springs by isotope and the noble gas method: case study of the Beljanica Massif
Earth-Surface Processes, Geology, Pollution, Soil Science, Water Science and Technology, Environmental ChemistryLjiljana Vasić, Laszlo Palcsu, Huang Fen. "Groundwater gravitational circulation of Karst Veliko Vrelo and Malo Vrelo springs by isotope and the noble gas method: case study of the Beljanica Massif" in Environmental Earth Sciences, Springer Science and Business Media LLC (2019). https://doi.org/10.1007/s12665-019-8294-0
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The Flow Conditions in the Epikarst Zone of a Karst Aquifer. Case Study: Suva planina Mt., East Serbia
Branislav Petrović (2023)The epikarst as a part of the karst aquifer represents a complex point of contact and mixing of unconsolidated material from the terrain surface, carbonate rocks altered by “corrosive” water, flora and fauna (and remains of), which is partially saturated with groundwater. Significant amounts of (plant accessible) water, and other solutes and particles, can be stored in this zone for extended periods of time. Thus, attenuation or biochemical processes could start in this layer and change quality of infiltrated ...Branislav Petrović. "The Flow Conditions in the Epikarst Zone of a Karst Aquifer. Case Study: Suva planina Mt., East Serbia" in International Scientific Conference "Man and Karst 2022", CIRS - Centro Ibleo di Ricerche Speleo-Idrogeologiche (2023)
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Оцјена водопропусности понорске зоне Шуковићу (Цернићко поље) помоћу Лижоновог теста
One of the specificities of reservoirs forming in highly karstified terrains is reflected in the wide range of unknowns, specifically during reservoir formation, filling and operation. Unfortunately, despite complex research, many reservoirs constructed in karst terrains have problems with water losses from the reservoir to other aquifers due to ponor and ponor zones which are a common in the karst of Eastern Herzegovina. One of such zones is Šuković ponor located in the southern part of the Cerničko polje ...Петар Војновић, Саша Милановић, Љиљана Васић. "Оцјена водопропусности понорске зоне Шуковићу (Цернићко поље) помоћу Лижоновог теста " in Мултидисциплинарна конференција “Kарст 2022 - Значај, стање и перспективе коришћења и заштите ресурса у карсту", Српска академија наука и уметности (2022)
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Reconstruction of the Tethys' waning in the Balkans: New insights from Upper Cretaceous igneous formations and zircon provenance data
... Qur zircon provenance data from Upper Cretaceous sediments in the Sava-Vardar Zone offer new insights into the closure of the Tethys in the Balkans. Our data from Upper Cretaceous formations in the Sava-Vardar suture zone demonstrate thc presence of all sequences recognized in the basement units ...
... researchers propose that this collision occurred in the Late Jurassic', others argue it took place at the end of the Cretaceous along the Sava-Vardar Zone?. The latter hypothesis suggests that the Upper- Cretaceous Sava Ocean is a remnant of the youngest Tethyan oceanic rcalm, left behind after a ...
... geodynamic environment, and lifespan of the purported Cretaceous Sava Ocean. The central scientific question Wec address is whether the Sava-Vardar Zone represents: (i) a relic of the Neo-Tethyan Ocean that closed in the Upper Cretaceous, or (ii) a diffuse tectonic boundary between previously collided ...Dejan Prelević, Kristijan Sokol, Ana Mladenović, Violeta Gajić, Vladica Cvetković. "Reconstruction of the Tethys' waning in the Balkans: New insights from Upper Cretaceous igneous formations and zircon provenance data" in Fifth Congress of Geologists of the Republic of North Macedonia, Macedonian Geological Society (2024)
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New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)
Nevenka Đerić, Nataša Gerzina (2014)... , Jadar Block, Vardar Zone Western Belt, Western Serbia 1. INTRODUCTION Brežđe village is situated in Western Serbia, at the foothills of the Maljen Mountain. The geological setting of the area is extremely complicated, considering the fact that this is a contact zone between the continental ...
... is referred to as the Vardar Zone Western Belt (KARAMATA, 2006), but also referred to under a variety of names such as the Inner Dinar- idic Ophiolite belt (LUGOVIĆ et al., 1991), the External Vardar Subzone (DIMITRIJEVIĆ, 1997, 2001) or simply the Vardar Zone (PAMIĆ et al., 2002). There are ...
... —— . | “Europe: north of the Vardar Zone Western Belt. It is considered (by incl. Serbo-Macedonian Massif the majority of Serbian geologists) to be either an integral Figure 1: Tectonic sketch of the Dinarides, modifted after SCHMID et al. part ofthe Vardar Zone (DIMITRIJEVIČ 1997) or an exotic ...Nevenka Đerić, Nataša Gerzina. "New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)" in Geologia Croatica (2014)
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Хидрогеолошке карактеристике изворишта за водоснабдевање Kањиже
Vladimir Jović ( 2024)Rad se bavi hidrogeoloskim karakteristikama izvorista za vodosnabdevanje opstine Kanjiza. Istrazivanja su sprovedena na tri hidrogeoloska kompleksa, od kojih su drugi i treći kompleks kljućni za vodosnabdevanje. Ovi kompleksi se nalaze u sedimentima pleistoćenske i paludinske starosti, na dubinama od 60 do 260 metara, sa subarteskim nivoom vode. Ukupne rezerve podzemnih voda u okviru drugog i treć eg hidrogeoloskog kompleksa iznose 935 l/s, a klasifikovane su u dve kategorije: B i C1. Kvalitet podzemnih voda je stabilan i pripada ...... neuobličeni peskovi čine niži deo terena koji se sa uskim pojasom od 2-10 km proteže uz dinska uzvišenja i dolinske ravni. Istočno od Subotičke peščare i reke Kereš, prostire se zona neuobličenih peskova, uz državnu granicu sa Mađarskom do Horgoša. Eolske tvorevine sa „peskom vejavcem” leže preko fluvialnih ...
... ZAŠTITE PODZEMNIH VODA .... 8.1. Neposredna zona sanitarne zaštite-ZONA | .....................aaiaaaii e aaadaaaeaeeeeeettaanı 45 8.2. Uža zona zaštite- ZONA II .........a a a aaaaaaaaaaaaaaoaaaaaaaaaaaaaaaaaaatteot 46 8.3. Šira zona zaštite- ZONA III...............aaaaaaa a eanaeaeakakaeattaatakkate ...
... za zahvatanje voda. Pored ove dve zone određuje se i zona neposredne fizičke zaštite oko samog eksploatacionog bunara ili izvorišta, koje predstavlja prvu zonu. 8.1. Neposredna zona sanitarne zaštite-ZONA I U skladu sa doredbama Pravilnika neposrednu zonu zaštite izvorišta formirane su oko ...Vladimir Jović. Хидрогеолошке карактеристике изворишта за водоснабдевање Kањиже, 2024
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New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia
Miloš Velojić, Dina Klimentyeva, Quadt von, Marcel Guillong, Frank Melcher, Thomas Meisel, Dejan Prelević (2023)Miloš Velojić, Dina Klimentyeva, Quadt von, Marcel Guillong, Frank Melcher, Thomas Meisel, Dejan Prelević. "New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia" in Geološki anali Balkanskoga poluostrva, Beograd : Srpsko geološko društvo (2023). https://doi.org/10.2298/GABP230330004V
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Fluid Evolution of the Čukaru Peki Cu-Au Porphyry System (East Serbia) inferred from a fluid inclusion study
Borska metalogenetska zona, Timočki magmatski kompleks, fluidne inkluzije, porfirska ležišta bakra, masivni sulfidi, slani rastvori, ključanje fluidaVelojić Miloš, Jelenković Rade, Cvetković Vladica. "Fluid Evolution of the Čukaru Peki Cu-Au Porphyry System (East Serbia) inferred from a fluid inclusion study" in Geologia Croatica, Croatian Geological Survey (2020). https://doi.org/10.4154/gc.2020.14
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First paleomagnetic and magnetic anisotropy results from Montenegrо - the coastal area
... distinguished. The Dalmatian(South-Adriatic) zone is in the lowermost tectonic position and comprises shallow waterCretaceous carbonates, bauxites, Middle Eocene nummulitic limestones, transitional marls, andUpper Eocene flysch. It is thrusted over by the Budva zone characterized by deep water sedimentsof ...
... Triassic through Paleogene ages with tuffitic layers in the Ladinian. The uppermost unit is theHigh Karst zone developed in a carbonate platform environment from the Middle Triassic till theend of the Cretaceous. In this unit flysch sedimentation started after the K/T boundary.From the above units we ...
... drilled and oriented in situ a total of 248 samples representing ninelocalities from the Dalmatian, six from the Budva and five from the High Karst zone, respectively.The harder rocks were drilled with portable gasoline powered, the softer ones with an electric drill.The laboratory measurements, dem ...Emö Márton, Vesna Cvetkov, Martin Đaković, Vesna Lesić, Slobodan Radusinović. "First paleomagnetic and magnetic anisotropy results from Montenegrо - the coastal area" in General Assembly 2021, Europen Geosciences Union (2021)
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Reconstruction of the Tethys’ Waning in the Balkans
Dejan Prelević, Kristijan Sokol, Ana Mladenović, Violeta Gajić, Vladica Cvetković. "Reconstruction of the Tethys’ Waning in the Balkans" in 16th Alpine Workshop, European Geosciences Union (2024)
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Trace elements in pyrite from the Čukaru Peki porphyry Cu-high-sulfidation deposit, Serbia: implications for ore evolution in a polyphase hydrothermal system
Miloš Velojić, Viktor Bertrandsson Erlandsson, Frank Melcher, Peter Onuk, Rade Jelenković, Vladica Cvetković (2022)Porfirska ležišta bakra, Ležišta visoke sulfidacije, Pirit, Elementi u tragovima, Laserska ablacija, Timočki magmatski kompleks, Borska metalogenetska zonaMiloš Velojić, Viktor Bertrandsson Erlandsson, Frank Melcher, Peter Onuk, Rade Jelenković, Vladica Cvetković. "Trace elements in pyrite from the Čukaru Peki porphyry Cu-high-sulfidation deposit, Serbia: implications for ore evolution in a polyphase hydrothermal system" in Geologia Croatica (2022). https://doi.org/10.4154/gc.2022.25
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Tracking of the temporal dependency of fading of the human footprint temperature contrast
In certain situations, it is extremely important to determine the exact time “someone” entered or crossed the forbidden zone of a military or strategic installation, a red zone of radioactive, chemical, or biological contamination, a bank or similar structure. Standard security measures include ordinary video surveillance using cameras that operate in the visible range of the electromagnetic spectrum, as well commercial thermal imaging cameras [1, 2]. The paper presents the results of experiments that suggest another possible use of ...Stevan Đenadić, Ljubiša Tomić, Vesna Damnjanović, Darko Vasiljević, Danica Pavlović. "Tracking of the temporal dependency of fading of the human footprint temperature contrast" in VIII International School and Conference on Photonics, Belgrade, Serbia, 23-27 August 2021, Institute of Physics Belgrade (2021)
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Primena programa UVSZ pri zaštiti od miniranja
Primena energije eksploziva tj. miniranje, predstavlja osnovni način eksploatacije čvrstih mineralnih sirovina u rudarstvu. Miniranjem se postižu vrlo povoljni tehnoekonomski pokazatelji, koje nažalost prate i negativni efekti miniranja. U cilju zaštite životne sredine potrebno je za svaku radnu sredinu odrediti jednačinu oscilovanja stenske mase pri miniranju. Ova jednačina definiše promenu brzine oscilovanja stenske mase u zavisnosti od rastojanja, količine eksploziva, uslova izvođenja miniranja i geoloških karakteristika stenske... promena u stenskom masivu. Kod homogenih i izotropnih sredina mogu se razlikovati tri zone: 1. Zona mrvljenja - u ovoj zoni udarni talas na okolne stene vrši pritisak brzinom koja je ve a od brzine zvuka, pri emu u zoni oko eksplozije, na rastojanju ( – polupre nik eksplozivnog punjenja) dolazi do ...
... promena u stenskom masivu. Kod homogenih i izotropnih sredina mogu se razlikovati tri zone: 1. Zona mrvijenja - u ovoj zoni udarni talas na okolne stene vrSi pritisak brzinom koja je veca od brzine zvuka, pri Cemu u zoni oko eksplozije, na rastojanju (3=7}r (r — polupretnik eksplozivnog punjenja) dolazi ...
... stenski masiv. 2. Zona razaranja - javlja se na rastojanju ve em od . U ovoj zoni udarni talas je znatno oslabljen i kre e se brzinom zvuka. U okolnom stenskom materijalu izaziva naprezanja koja za posledicu imaju stvaranje pukotina razli itih pravaca i orijentacija. 3. Zona potresanja - nastaje ...Suzana Lutovac, Miloš Gligorić, Jelena Majstorović, Luka Crnogorac, Rade Tokalić. "Primena programa UVSZ pri zaštiti od miniranja" in XIII skup privrednika i naučnika SPIN’21, Industrija 4.0 – mogu nosti, izazovi i rešenja za digitalnu transformaciju privrede, Univerzitet u Beogradu, Fakultet organizacionih nauka (2021)
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Metalogenija južnog dela Vardarske zone
Tomislav Ivanov (1965)Tomislav Ivanov. Metalogenija južnog dela Vardarske zone, Beograd:Rudarsko Geološki Fakultet, 1965
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Konceptualni model hidrogeotermalnog sistema šire okoline Brusa - geotermalna karakterizacija sistema / Conceptual model of hydrothermal system of Brus area - system geothermal characterization
Dejan Milenić, Ana Vranješ, Marinko Toljić, Ivana Vasiljević, Natalija Radosavljević, Matija Ognjanović (2024)Postavljeni konceptualni model hidrogeotermalnog sistema Brusa sa širom okolinom testiran je primenom različitih hidrohemijskih i izotopskih metoda u cilju njegove verifikacije i karakterizacije. Rezultati su ukazali na atomsfersko poreklo geotermalnih fluida i na razviće primarnih rezervoara u okviru karbonatnih stena. Prvi rezervoar formiran je u okviru krečnjaka gornjotrijakse starosti, dok drugi rezervoar egzistira u okviru trijskaih mermera. Zone prihranjivanja locirane su u zapadnom delu terena. Sistemi gravitacionih raseda kontrolišu kretanje fluida u sistemu, dok proces jonske izmene dominira u ...Dejan Milenić, Ana Vranješ, Marinko Toljić, Ivana Vasiljević, Natalija Radosavljević, Matija Ognjanović. "Konceptualni model hidrogeotermalnog sistema šire okoline Brusa - geotermalna karakterizacija sistema / Conceptual model of hydrothermal system of Brus area - system geothermal characterization" in XVII Srpski simpozijum o hidrogeologiji sa međunarodnim učešćem , Pirot, Serbia, 02-06. October 2024, Beograd : Univerzitet u Beogradu - Rudarsko-geološki fakultet (2024). https://doi.org/10.5281/zenodo.13739443
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Metalogenija zone Mačkatica-Blagodat-Karamanica
Milosav Simić (1996)Milosav Simić. Metalogenija zone Mačkatica-Blagodat-Karamanica, Beegrad:Rudarsko Geološki Fakultet, 1996
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Ocena efektivnosti geoloških istraživanja u zoni jugoistočno od Bora
MIodrag Miličić (1977)MIodrag Miličić. Ocena efektivnosti geoloških istraživanja u zoni jugoistočno od Bora, Beograd:Rudarsko-geološki fakultet, 1977
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Geološka građa terena limske zone između Prijepolja i jabuke
Aleksandar Ž. ILIĆ (2000)Aleksandar Ž. ILIĆ. Geološka građa terena limske zone između Prijepolja i jabuke, Beograd:Rudarsko-geološki fakultet, 2000
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Genetski tipovi magnezitskih ležišta u zoni ultrabazita Dinarida
Miloje Ilić (1964)Miloje Ilić. Genetski tipovi magnezitskih ležišta u zoni ultrabazita Dinarida, Beograd:Rudarsko Geološki Fakultet, 1964
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Metalogenija antimona u reonu Kostajnica(antimonska zona Podrinja)
Jovica Milčić (1982)Jovica Milčić. Metalogenija antimona u reonu Kostajnica(antimonska zona Podrinja), Beograd:Rudarsko-geološki fakultet, 1982