Претрага
826 items
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Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia
Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić (2022)The paper compares the flow regimes of the Resava River at the gauging stations of the Manasija Monastery (upper course) and the town of Svilajnac (lower course). The hydrological analysis encompasses a multiyear period of monitoring (1982–2020). The water budget and baseflow index are assessed for the catchment areas monitored by the Svilajnac station (683 km2) and the Manasija Monastery station (358k m2), considering the overall monitoring period and characteristic years. The results indicate that the specific runoff in ...... SBSBSSBS BBB R B B G B BBB a dii 0 š . a bvu.ž·ižšjžrgozn |—g.s. at Manasija Monastery —-g:5. at Svilajnac |—C-g5. at Manasija Monastery —-g.5. at Svilajnac • 180 . 160 s s o : z a : o g 10 P Ž ž Š w š š k i 33 Š o |}] E 40 || > o LJ 2808 888 8#8.8#8.4. 8 + žž BII II I I ŠGU 39 8B B ! Š Š 9 ž ...
... ž Š Š Š 3 'B B ! Š BI B R BO Cju.=<21”·(3320 d BB BSKSSBIBISB IBE —. at Manssin Mopasisty ——g:s. atvisjne ——>s at Manasija Monastery —-g.s. at Svilajnac Fig. 1. Catchment of the Resava River and parallel discharge hydrographs of characteristic years: (q) and (b) years in which the mean annual discharge ...
... covered by the gauging stations is 1:1.75. This sug- gests that most of the discharge of the Resava River is formed in the upper catchment (Figs. 1a,b). In the case of the characteristic low mean annual dis- charge, thc ratio was 1:0.57 in 1994, meaning that during dry periods the annual discharges ...Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić. "Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia" in National Conference with International Participation “GEOSCIENCES 2022”, Sofia : Bulgarian geological society (2022)
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Препреке декарбонизацији система даљинског грејања у Србији - ставови представника топлана
Производња топлоте у системима даљинског грејања у Републици Србији тренутно се заснива искључиво на процесима сагоревања, с доминантним уделом природног гаса из увоза. Иако су технологије за коришћење обновљивих и алтернативних извора енергије добро познате, њихова примена у системима даљинског грејања у Републици Србији још увек је занемарљива (око 2%). Како би се убрзао и олакшао процес транзиције ка обновљивим изворима енергије и разумело тренутно стање и перспектива, спроведена је анкета међу представницима топлана Србији. Циљ је био ...Марија Живковић, Дејан Ивезић, Бобан Павловић, Дејан Стојановић. "Препреке декарбонизацији система даљинског грејања у Србији - ставови представника топлана" in Стручно-научна конференција ТОПС 2024, Златибор, Јун 2024, Пословно удружење "Топлане Србије" (2024)
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Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications
The Vardar-Tethyan mega-suture between the Eurasian and Adria (Gondwana) margins comprises remnants of oceanic lithosphere of Neotethys and distal parts of the adjacent continental margins including unconformable Late Cretaceous sedimentary cover and Cenozoic igneous rocks of post-obduction age. This study provides kinematic constraints for displacements and rotations affecting the Serbian part of the West Vardar and Jadar-Kopaonik units after the closure of the Neotethyan (= Sava) Ocean. The targets of the paleomagnetic research were Late Cretaceous sediments representing an ...... in te rp re ta ti o n ar e in b o ld R em ar k s: L o ca li ty 1 : sa m p le s le ft o u t ar e m o st li k el y th e re -d ep o si te d sh al lo w w at er ca rb o n at es w it h n eg at iv e su sc ep ti b il it y ei th er sc at te re d d ir ec ti o n s o r b ad d em ag n et iz at io n cu rv ...
... al . 2 0 1 5 ). T h e ag e d et er m in at io n w as d o n e b y M il en a D u n či ć b as ed o n w el l p re se rv ed m ic ro fo ss il as so ci at io n s ex ce p t fo r lo ca li ti es 4 an d 8 w h er e th e ag e is fr o m th e B as ic G eo lo g ic al M ap o f fo rm er Y u g o sl av ia 202 ...
... Pavlović, Z., Marković, B., Rodin, V., Marković, O., Gagić, N., et al. (1976). Basic Geological Map of SFRJ, sheet Gornji Milanovac (scale 1:100 000). Beograd: Savezni Geološki Zavod. Filipović, I., Rodin, V., Pavlović, Z., Marković, B., Milićević, M., & Atin, B. (1979). Basic Geological ...Vesna Lesić, Emo Márton, Violeta Gajić, Dragana Jovanović, Vesna Cvetkov. "Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications" in Swiss Journal of Geosciences, Basel : Springer International Publishing (2018). https://doi.org/10.1007/s00015-018-0321-8
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Geotermalne karakteristike područja Semberije , Republika Srpska
Igor Glavaš (2024)Cilj završnog rada predstavlja, opis geotermalnih karakteristika područja Semberije, Republika Srpska, BiH.Rad se sastoji od opšteg dijela u kojem se navode osnovne karakteristike područja (geomorfološke, geografske, hidrološke,hidrometeorološke, geološke, tektonske i hidrogeološke) i specijalnog dijela koji detaljnije ulazi u tematiku osobina geotermalne energije i njihovih karakteristika u zadatom području kao i definisanje geotermalnog potencijala koje to područje ima.Sa prognoznim litološkim profilima 6 dubokih istražnih bušotina su izrađena 2 regionalna geološka, a njegovom konverzijom i hidrogeološka profila na osnovu kojih je, stečena ...... „Dvorovi“, koji se još koristi i u balneološke svrhe. U upotrebi postoji ı manji broj plitkih bunara koji eksploatišu subhidrogeotermalni resurs (B-1, B-2 i B-3). Uticaj efekta „toplotnog ostrva“ na podzemne vode istražnog područja nije ustanovljen u sklopu najvećeg centra (Bijeljina) sa mjerenjima ...
... dubine su dobijene intervjuisanjem vlasnika objekta, što može dovesti do nesigurnosti ovog podatka. Bunari B-1 (stambena zgrada u Jermenskoj), B-2 (bunar izrađen metodom laviranja TC „Tropik“) i B-3 (bunar sa toplotnom pumpom u okviru Doma zdravlja Bijeljina) su bušeni bunari čija je svrha 31 ...
... sledećem grafiku: Prosječne padavine i temperatura područja u periodu 2010-2021. godine 30 150 — B 20 100 Š | a [} |= % 10 50 Š [ a Š -| 0 0 « % < S I ) + I « + & & K (šac@b “OMB 0 O „ i O»@@ i ii a & I Oz. m Padavine , —Temperatura Slika 2.1. Srednje mjesečne temperature i ...Igor Glavaš. Geotermalne karakteristike područja Semberije , Republika Srpska, 2024
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Nelinearno dinamičko modelovanje potresa izazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija
Srđan D. Kostić (2013-11-04)U ovoj disertaciji, cilj istraživanja bio je određivanje dinamičkih svojstava potresaizazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija.Analiza potresa izvedena je sa dva aspekta – u prvom delu istraživanja izučavane suvremenske serije oscilovanja tla za vreme potresa, a u drugom delu vršena je analizastabilnosti fenomenološkog Baridž-Knopof modela bloka sa oprugom. Vremenske serijeoscilovanja tla proučavane su primenom postupka analize surogat podataka, kao ikorišćenjem metoda analize nelinearnih vremenskih serija (primena teoreme orazvijanju skalarne vremenske serije). Analiza vremenskih serija izvedena je ...potres, naponsko stanje, podzemne prostorije, bifurkacije, vremenskaserija, deterministički haos, stohastičnost, perturbacije, vremensko kašnjenje, jačina trenja... gde je PA(a) verovatnoća osmatranja vrednosti a u skupu svih vrednosti sistema A, PB(b) – verovatnoća osmatranja vrednosti b u skupu svih vrednosti sistema B, i PAB(a,b) zajednička verovatnoća merenja a i b. Veličina I naziva se uzajamna informacija dva merenja ai i bk, i simetrična je, u smislu ...
... ln 0 0 0 c VV V A B V D (4.6) Parametri A i B su empirijske konstante. Prema [Rice, 1993, 2001], parametar A predstavlja meru direktne zavisnosti od brzine (koja se ponekad naziva ,,direktni efekat’’), dok je (A – B) mera zavisnosti trenja ...
... ))(),(( log))(),(()( (6.13) gde je I(τ)≥0 (Gallager, 1968). Kada su merenja sistema A i B potpuno nezavisna, tada je PAB(a,b)=PA(a)PB(b), i IAB(ai,bk)=0. Nakon određivanja distribucije I(τ) postavlja se pitanje: koju vrednost I(τ) možemo koristiti za rekonstrukciju ...Srđan D. Kostić. "Nelinearno dinamičko modelovanje potresa izazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2013-11-04)
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Nelinearno dinamičko modelovanje potresa izazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija
Srđan D. Kostić (2013-11-04)U ovoj disertaciji, cilj istraživanja bio je određivanje dinamičkih svojstava potresaizazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija.Analiza potresa izvedena je sa dva aspekta – u prvom delu istraživanja izučavane suvremenske serije oscilovanja tla za vreme potresa, a u drugom delu vršena je analizastabilnosti fenomenološkog Baridž-Knopof modela bloka sa oprugom. Vremenske serijeoscilovanja tla proučavane su primenom postupka analize surogat podataka, kao ikorišćenjem metoda analize nelinearnih vremenskih serija (primena teoreme orazvijanju skalarne vremenske serije). Analiza vremenskih serija izvedena je ...potres, naponsko stanje, podzemne prostorije, bifurkacije, vremenskaserija, deterministički haos, stohastičnost, perturbacije, vremensko kašnjenje, jačina trenja... gde je PA(a) verovatnoća osmatranja vrednosti a u skupu svih vrednosti sistema A, PB(b) – verovatnoća osmatranja vrednosti b u skupu svih vrednosti sistema B, i PAB(a,b) zajednička verovatnoća merenja a i b. Veličina I naziva se uzajamna informacija dva merenja ai i bk, i simetrična je, u smislu ...
... ln 0 0 0 c VV V A B V D (4.6) Parametri A i B su empirijske konstante. Prema [Rice, 1993, 2001], parametar A predstavlja meru direktne zavisnosti od brzine (koja se ponekad naziva ,,direktni efekat’’), dok je (A – B) mera zavisnosti trenja ...
... ))(),(( log))(),(()( (6.13) gde je I(τ)≥0 (Gallager, 1968). Kada su merenja sistema A i B potpuno nezavisna, tada je PAB(a,b)=PA(a)PB(b), i IAB(ai,bk)=0. Nakon određivanja distribucije I(τ) postavlja se pitanje: koju vrednost I(τ) možemo koristiti za rekonstrukciju ...Srđan D. Kostić. "Nelinearno dinamičko modelovanje potresa izazvanih promenom naponskog stanja pri izradi horizontalnih podzemnih prostorija" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2013-11-04)
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Two approaches to compilation of bilingual multi-word terminology lists from lexical resources
In this paper, we present two approaches and the implemented system for bilingual terminology extraction that rely on an aligned bilingual domain corpus, a terminology extractor for a target language, and a tool for chunk alignment. The two approaches differ in the way terminology for the source language is obtained: the first relies on an existing domain terminology lexicon, while the second one uses a term extraction tool. For both approaches, four experiments were performed with two parameters being ...Branislava Šandrih, Cvetana Krstev, Ranka Stanković. "Two approaches to compilation of bilingual multi-word terminology lists from lexical resources" in Natural Language Engineering, Cambridge University Press (CUP) (2020). https://doi.org/10.1017/S1351324919000615
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Fuzzy stohastički model izbora sistema otvaranja podzemnog rudnika
Saša M. Jovanović (2016-05-16)Investiciono okruženje skopčano sa rudarskom industrijom je veoma svojstveno kada seuporedi sa okruženjima koje susrećemo u tipičnim proizvodnim industrijama. Neke odkarakterisitka rudarstva, koje su često naznačene kao jedinstvene su: visok intenzitetinvesticija, dugi predproizvodni periodi, visok rizik i neobnovljivost resursa.Investiranje u sistem otvaranja rudnika predstavlja dobar primer ireverzibilneinvesticije. Takva investicija zahteva pažljivu analizu, jer nakon njene realizacije ona sene može nadoknaditi bez značajnog gubitka vrednosti. Očigledno je da izbor sistemaotvaranja podzemnog rudnika pripada strateškom planiranju...... m 8 m 84 6 95 7 1 7 .44 B K -3 /9 0 7 8 1 .97 B K -1 3 /90 7 10 .39 B -10 /90 7 09 .3 B K -4 /9 0 7 32 .53 B -1 /8 9 701 .4 B K -8 /90 7 20 B K -9 /9 0 B K -5 /9 0 B 6 5 B 15 5 B 15 9 B 1 52 7 6 5 .34 B K -2 /9 0 7 28 B K -1 4 /9 0 vb b b 2 2 to lo w e r le ve l lo ad ...
... 590 600 610 620 630 640 650 660 720 730 740 750 760 770 510 500 670 680 690 700 710 490 780 480 790 470 B-28 B-140 K-4 B-24 B-129 B-22 B-127 B-21 S-598 S-590 S-582 S-574 S-566 S-558 S-550 S-542 S-534 S-526 S-518 S-510 S-502 S-494 S-486 S-670 S-662 S-654 ...
... 590 600 610 620 630 640 650 660 720 730 740 750 760 770 510 500 670 680 690 700 710 490 780 480 790 470 B-28 B-140 K-4 B-24 B-129 B-22 B-127 B-21 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 S-598 S-590 S-582 S-574 ...Saša M. Jovanović. "Fuzzy stohastički model izbora sistema otvaranja podzemnog rudnika" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2016-05-16)
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Proračun kapaciteta bagera u selektivnom radu na Pk ,,Drmno
Dušan Stanisavljević (2024)U ovom Završnom radu obrađena je problematika proračuna kapaciteta bagera u površinskoj eksploataciji ležišta mineralnih sirovina. Dat je prikaz opštih karakteristika i načina rada rotornih bagera, kao i proracun kapaciteta bagera u selektivnom radu na PK ,,Drmno,,. Urađena je analiza dobijenih rezultata I izveden krajinji zaključak iz istih.... 18 ; . ( ) o Šav = arc sin = arc sm = 25 . {B 59,6 — 45,96 + 7,42 š = arc sin —) = 279 B_BM +4Wb R +4 ly . ( = arc sin 46,97 Šv = arc sin( B, - R +A ln Ig 59,6 — 45,96 + 16,17 . ( ) o Šoer = arc sin =arc sih |_L_——————|=40 Ruvu 46,36 B, -R +4 ly; j (59,6 — 45,96 + 13,12) _ 3go = arc ...
... Prva linija formirana je od transportera 10 U-I-1 i U-I-2 ( B-1800mm ) i omogućava otkopavanje od zapadne do istčne granice, odnosno celom fronta radova na uglju. Drugu liniju etažnih transportera čini samo transporter U-I-4 ( B-1800mm ), dok je formiranje transportera U-I-3 u planu. Etažni ...
... (ž) = 40? 46,36 uVI Ugao zaokretanja strele prema spoljašnjoj bočnoj kosini, osim poslednje donje: B,R +A l ___/59,6 — 45,96 + 0 ——— | = qTC SIn (—) = 17? Š = arc sm( F3 45,96 ul _ (B,-R, +Al | _/59,6 — 45,96 + 3,04 šai = arc sin| —c— _J= arc sin (—) = 21? Ruu 46,55 - R +A lii . 59,6 ...Dušan Stanisavljević. Proračun kapaciteta bagera u selektivnom radu na Pk ,,Drmno, 2024
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Услови заштите изворишта подземних вода “Јарош“ за водоснабдевање Сомбора
Ивана Јовановић (2024)Територија града Сомбор се налази у периферном северозападном делу Војводине, односно Србије, у близини границе са Хрватском. Сам град Сомбор се налази југозападном делу територије и представља гравитациони центар тог подручја. Повољан географски положај условио је афирмацију Сомбора као градског насеља, са јаком пољопривредом, индустријом, занатством и прометом. "ВОДОКАНАЛ" из Сомбора је јавно комунално предузеће чија је основна делатност захват сирове подземне воде, њен третман, и дистрибуција ка потрошачима Сомбора и приградских насеља и насељених места: Лугова, Жарковца, Чонопље, ...... H3BOpHmrma “Japomi“ je TpeHyrIHO V eKcnmoaTamnjH 18 eKcrimoaTauHoHHXx o0jeKaTa — OyHapa caenehHx o3Haka: 5-1A, B-2A. b-3A., 5-4A. b- 5A. b-6A. b-7A. 5b-SA. 5-9. 5-10. 5-11A. b-12. 5-13. b-14A. 5-15, 5-16. 5-18 H H-3, a KOJH KaTITHpajy IIpBy H3J1aHCKy 3OHy, CuKO O u ma0ena 3. Ta6e.na 5. ExcnnoamauyuouHu ...
... oyHapnHMa B-2a, B-6a, 5-7a, 5-8a, 5-11a, 5-12, 5-15 H 5-16 Mepaun rnporoka HHcy y byHKuHjHt (y KBapy, He nocTajy...), a KonHuHHe Hnon3eMHe BORe Koja ce ekcnnoaTHIHe H-HMa yna3e y CyMapHH KamanHTeT KojH perHcTpyje 30HpHH Mepau rnpe ynacKa y d a6pnky Bo,ate. T i v j e s o v e Y T a p c k v ı M B O ...
... OKDVOCYJe, TIipocrop H3BopHmrra „Japomi“ je cacraB;beH IIpOCTOpHO 0J1 ;TBa JTeza: "crapo" no:be Koje uHHe eKC:1OaTaLHIHOHH OyHapH 5-1A. b-2A. 5-3A. 5-4A. b- 5SA. 5-6A. b-7A. 5b-šA H H-3 "HOBO" IIO-be Ha KOMe Ce Hajna3e OyHapH 5-9. 5-10. 5-11A . 5-12. 5-13. 5-14A. 5-15. 5-16 H 5-18 „Crapo“ rozmbe ...Ивана Јовановић. Услови заштите изворишта подземних вода “Јарош“ за водоснабдевање Сомбора, 2024
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Application of machine learning for diagnosing the operation of a deep well pump in oil production
Maja Trikić (2024)This paper will thoroughly examine how machine learning can improve the diagnosis of deep well pumps by analyzing the role and function of the pumps, dynamograms, sensor technologies, and diagnostic methods.Our analysis will provide insights into modern techniques and approaches for enhancing the performance and reliability of oil production systems, targeting cost reduction and increased operational efficiency.deep well pump, dynamograms, machine learning, diagnostics of operating coditions,Random Forest, XGBoost... tion process. The schema for classifying background logs used in this study is shown in Figure 6.9. Specialist Standard cards „ S 5 5 B B B E B B B E B B E E -f. „O F Store cards V I V I I I I I ) Card visualization Label cards Discard cards Figure 6.9. Classification and manual selection ...
... Continuous Wavelet Transform, described by equation (13). _ k-b Cw(s,b) = .J z(k)QC2-)dk (13) where: Cw(5, b)- is the result of the wavelet transform, Z(k)- is the signal being analyzed, iW)((k — b)/s)- is the wavelet function, s and b-scale and translation 54 The main difference between ...
... 12 b o ' Li L “ [] LJ ? LI vromoe (%5e0C}) Figure 3.1 time functions of load and stroke of the smooth rod Š·o i E PR N a a m e .'! ” L A_'A––––Ev @llšsss·zlll B dı | | | oO e % 2 «0 bl · tod glatko Sipko S(cm) Figure 3.2 Dynamograms of downhole pump operation: a})load, b)surface ...Maja Trikić. Application of machine learning for diagnosing the operation of a deep well pump in oil production, 2024
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Trace elements and garnet formation in a distal skarn zone: a case study of the Rudnik deposit, Central Serbia
Bojan Kostić, Pavle Tančić, Natalija Batoćanin. "Trace elements and garnet formation in a distal skarn zone: a case study of the Rudnik deposit, Central Serbia" in Geological Quarterly, septembar 2024, Polish Geological Institute - National Research Institute (PGI-NRI) (2024). https://doi.org/10.7306/gq.1752
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Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations
The type of dip-slip faults can be assessed based on the analysis of vertical gravity gradients. Theoretically, just a simple comparation of the gradient extreme values can give us an answer whether the fault is normal or reverse (thrust). Practical application of this method is far more complicated and the results depend on a number of parameters, such as a complexity of geological setting, the quality of gravity data, dip angle and displacement of the fault, density contrast, etc. ...... 14 South Morava x [km] Fla FIb F2a F2b River F3 F4 i i vi < VOA - K i (b) s VOA V X V a \ c u Figure 3. Field example from South Morava trench: (a) vertical gravity gradient (Uzz) curves A, B and C and (b) disposition of the faults obtained from geological data (red dashed and full lines ...
... North Macedonia 3BOPHHK HA TPYJOBU PROCEEDINGS * a eS 4 e* - + BI bLAHIA ~ b. Seratimovski, T. & Boey, B. Oxpud, 2024 / Ohrid, 2024 TJloce6no us0aHue Ha Geologica Macedonica,M 6 MAKEJ/IOHCKO TEOJIOIHHKH JIPVIHITBO CKOTIJE 1952 MACEDONIAN ...
... Geologists of the Republic of North Macedonta 3BOPHMHK HA TPYVJIOBMH PROCEEDINGS ypeonuuu / Editors: Cepa()HMoBcku, T. & BoeB, B. Serafimovski, T. & Boev, B. Oxppin, 2024 / Ohrid, 2024 MHynraBau: MakeJIOHCKO TČOJIOHIKO JIpyITTBO IynaBHH H 0JIT0OBOpHu ype/iHuHiH IIpoQ. m-p Tonop Cep ...Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković. "Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations" in Vth Congress of the Geologists of the Republic of North Macedonia, Ohrid, Republic of North Macedonia, September 27-28, 2024, Macedonian Geological Society (2024)
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Numerical modeling of Selanac debris flow propagation using SPH code
The Selanac debris flow is a very huge event triggered after extreme rainfall caused by Cyclone Tamara activity in the Republic of Serbia in May 2014. The Selanac case study was already modelling in different programs using Voellmy rheology assumptions like RAMMS software. In this paper research are focusing particularly on the process of debris flowing from initiation zone to main deposition area using Geoflow SPH two-phase model considering frictional rheology law. Main rheological parameters are back-calculated using also ...... 15th-19th-2020 Figure 3 Final model of flow heights A) 16s B) 30s C) 50s D) 100s SCG-XIII INTERNATIONAL SYMPOSIUM ON LANDSLIDES. CARTAGENA, COLOMBIA- JUNE 15th-19th-2020 Figure 4 Erosion depths in meters in time steps A) 16 s B) 30 s C) 50 s D)100 s 5 CONCLUSIONS Final models show ...
... I., Mira, P., González, E., Haddad, B., Quecedo, M., Tonni, L., Drempetic, V. (2008) ‘’Mathematical, constitutive and numerical modelling of catastrophic landslides and related phenomena’’. Rock Mech Rock Eng 41:85–132. Pastor, M., Blanc, T., Haddad, B. et al. (2014). ‘’Depth Averaged Models ...
... which stands among the largest occurrence of this type of landslides recorded in Serbia, recently (Fig. 1). Figure 1 A) UAV image of main scarp B) UAV image of transportation zone The Selanac debris flow is a complex flow type landslide phenomenon, firstly triggered as slide of huge initial ...Jelka Krušić, Biljana Abolmasov, Miloš Marjanović, Manuel Pastor, Saeid M. Tayyebi . "Numerical modeling of Selanac debris flow propagation using SPH code" in SCG-XIII International Symposium on Landslides. Cartagena, Colombia- February 22-26, 2021, International Society for Soil Mechanics And Geotechnical Engineering (2021)
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Analysis and visualization of geophysical well-logging data from closely spaced boreholes
Geophysical logging measurements for determining the condition of the rock mass on the dam profile and locating the predisposed directions of water circulation and loss from the reservoir were conducted in four boreholes distributed at a close distance. The survey was carried out in a typical karst terrain, which is an additional challenge for defining the geological model, especially in terms of water retention. That kind of data set provides an excellent opportunity for a new approach to analysis ...Branislav Sretković, Ivana Vasiljević, Dimitry Sidorov - Biryukov. "Analysis and visualization of geophysical well-logging data from closely spaced boreholes" in Vth Congress of the Geologists of the Republic of North Macedonia, Ohrid, Republic of North Macedonia, September 27-28, 2024, Macedonian Geological Society (2024)
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Fluid inclusion systematics in the Okoška gora polymetallic deposit
... the Sheet Slovenj Gradec. Federal Geological Survey Belgrade, 74 pp. Schmid, S. M., Fiigenschuh, B., Kounov, A., Matenco,L., Nievergelt, P.. Oberhinsli, R., Picuge Schefer, S., Schuster, R., Tomljenovič, B., Ustaszewski, K.. & van Hinsbergen, U. 3. J, 2 Tectonic units of the Alpine collision zone between ...
... Geologists ODDELEK ZA GEOLOGIJO Ljubljana 2021 јапак, M., Froitzheim, N., Luptak, B., Vrabec, M, & ultrahigh-pressure metamorphism of eclogites subduction in the Eastern Alps, Slovenia. • T. Linnemann, U., Ouzegane, K., Drareni, A ...
... Precambrian Research, 224, 236–278. Mioč, P. 1972: Basic Geological Map of Yugoslavia 1:100.000.5 to the Sheet Slovenj Gradec. Federal Geological Survey B Sigesmund,S., Oriolo, S., Heinrichs, T.. Basei, M. A. S., Nolte, N 2018: Provenance of Austroalpine basement metasedimenits: connections between p ...Aleš Šoster, Miloš Velojić, Barbara Potočnik Krajnc, Matej Dolenec. "Fluid inclusion systematics in the Okoška gora polymetallic deposit" in 25th meeting of Slovenian geologists, Ljubljana, 2021, Univerza v Ljubljani, Oddelek za geologijo (2021)
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An arid phase in the Internal Dinarides during the early to middle Miocene: Inferences from Mg-clays in the Pranjani Basin (Serbia)
N. Andrić-Tomašević, V. Simić, O. Mandic, D. Životić, M. Suárez, E. García-Romero. "An arid phase in the Internal Dinarides during the early to middle Miocene: Inferences from Mg-clays in the Pranjani Basin (Serbia)" in Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier BV (2020). https://doi.org/10.1016/j.palaeo.2020.110145
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Multihazard Exposure Assessment on the Valjevo City Road Network
Miloš Marjanović, Biljana Abolmasov, Svetozar Milenković, Uroš Đurić, Jelka Krušić, Mileva Samardžić Petrović (2019)Miloš Marjanović, Biljana Abolmasov, Svetozar Milenković, Uroš Đurić, Jelka Krušić, Mileva Samardžić Petrović. "Multihazard Exposure Assessment on the Valjevo City Road Network" in Spatial Modeling in GIS and R for Earth and Environmental Sciences, Elsevier Inc (2019). https://doi.org/10.1016/B978-0-12-815226-3.00031-4.
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Nonequilibrium athermal random-field Ising model on hexagonal lattices
Svetislav Mijatović, Dragutin Jovković, Đorđe Spasojević. "Nonequilibrium athermal random-field Ising model on hexagonal lattices" in Physical Review E, American Physical Society (APS) (2021). https://doi.org/10.1103/PhysRevE.103.032147
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Heavy metals in lignite and soil of Kostolac-Kovin coal basin, eastern Serbia - comparative analysis with selected cities in Serbia, region, Europe and world
Bogoljub Vučković, Bojan Dimitrijević (2023)The Kostolac-Kovin coal basin with an area of 320 km2, with 5 separate layers of coal and with a total of about 5.7 Bt of geological resources and reserves represents an exceptional potential for coal production in Serbia. The coal resources listed in this way are not fully exploitable, but they represent potential for consideration. In this paper, we deal with the geochemical characteristics of coal seams and perform a comparative analysis of coal affectation on the environment. With ...... L., Grinstein M., Liu Y., Green K., Wai W., Wazed B., Shaw R., 2015 – Trace Metal Contamination in New Vork City Garden Soil - Soil Sci 180, Technical article 8. Chonokhuu S., Batbold C., Chuluunpurev B., Battsengel E., Dorjsuren B., Byambaa B., 2019 - Contamination and health risk assessment ...
... 00075100007512000751400075100007518000752000075220007523000 b) d) Figure 3. General view of the spatial distribution of 5 separate coal seams in the Kostolac-Kovin coal bearing basin – a) I (red dots) and I (pink dots) coal seams; b) II (black dots) coal layer; c) la coal layer; d) IP coal layer ...
... from coal, 45 from ash, 165 from gravel and 30 from soil, we perform analysis of horizontal and vertical distribution of HM and comparative analysis. B/hat interests us as authors and you as readers the most is - whether heavy metals from coal contaminate the accompanying sediments above and around ...Bogoljub Vučković, Bojan Dimitrijević. "Heavy metals in lignite and soil of Kostolac-Kovin coal basin, eastern Serbia - comparative analysis with selected cities in Serbia, region, Europe and world" in 9th International Conference Mining and Environmental Protection, 24–27. May 2023, Sokobanja, Beograd : Univerzitet u Beogradu, Rudarsko-geološki fakultet (2023)