Претрага
782 items
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Analogue modelling of strain partitioning along a curved strike-slip fault system during backarc-convex orocline formation: Implications for the Cerna-Timok fault system of the Carpatho-Balkanides
Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović (2021)... models. J. Struct. Geol. 28, 421–430. Limberger, J., Calcagno, P., Manzella, A., Trumpy, E., Boxem, T., Pluymaekers, M.P.D., van Wees, J.-D., 2014. Assessing the prospective resource base for enhanced geothermal systems in Europe. Geoth. Energ. Sci. 2, 55–71. Limberger, J., van Wees, J.-D., Tesauro ...
... interaction. J. Terramechanics 50, 311–326. Smit, J., Brun, J.-P., Cloetingh, S., Ben-Avraham, Z., 2008. Pull-apart basin formation and development in narrow transform zones with application to the Dead Sea Basin. Tectonics 27, TC6018. https://doi.org/10.1029/2007TC002119. Smit, J., Brun, J.-P., Cloetingh ...
... 17 Dahlen, F., Suppe, J., Davis, D., 1984. Mechanics of fold-and-thrust belts and accretionary wedges: Cohesive Coulomb theory. J. Geophys. Res. 89 (B12), 10087–10101. Davis, D., Suppe, J., Dahlen, F.A., 1983. Mechanics of fold-and-thrust belts and accretionary wedges. J. Geophys. Res. 88 (B2) ...Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović. "Analogue modelling of strain partitioning along a curved strike-slip fault system during backarc-convex orocline formation: Implications for the Cerna-Timok fault system of the Carpatho-Balkanides" in Journal of Structural Geology, Elsevier BV (2021). https://doi.org/10.1016/j.jsg.2021.104386
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Tehnološki aspekti izrade lateralnih bušotina kratkog radijusa
Vladimir J. Žuža (2006)Vladimir J. Žuža. Tehnološki aspekti izrade lateralnih bušotina kratkog radijusa, Beograd:Rudarsko-geološki fakultet, 2006
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Effectiveness Analysis of Different Bucket-wheel Excavators
Coal production in open-pit lignite mines in the Republic of Serbia is performed with continuous work systems. In addition to coal production, the same systems are used for the exploitation of large quantities of overburden. According to the reliability concept, continuous systems are in linear connection. If the failure occurs in one part of the system, that will produce a downtime of the entire system. The initial and most important factor of continuous systems is the bucket-wheel excavator. It ...Stevan Đenadić, Predrag Jovančić, Dragan Ignjatović, Miloš Tanasijević, Filip Miletić. "Effectiveness Analysis of Different Bucket-wheel Excavators" in 8th International Conference Mining and Environmental Protection, Sokobanja, 22-25 September 2021, University of Belgrade, Faculty of Mining and Geology, Belgrade, Serbia (2021)
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Some examples of interactions between certain rare earth elements and soil
... REFERENCES 1. I. Anastopoulos, A. Bhatnagar, E. C. Lima, J. Mol. Liq. 221 (2016) 954 (https://doi.org/10.1016/j.molliq.2016.06.076) 2. F. Tommasi, P. J. Thomas, G. Pagano, G. A. Perono, R. Oral, D. M. Lyons, M. Toscanesi, M. Trifuoggi, J. Arch. Environ. Contam. Toxicol. 81 (2021) 531 (https://doi ...
... editing process and publishing procedure applied by the JSCS Editorial Office. Please cite this article as Z. Nikolovski, J. Isailović, D Jeremić, S. Kovač, I. Brčeski, J. Serb. Chem. Soc. (2021) https://doi.org/10.2298/JSC211006095N This “raw” version of the manuscript is being provided to ...
... (https://doi.org/10.1007/s00244-020-00773-4) 3. V. Balaram, J. Geosci. Front. 10 (2019) 1285 4. V. M. Goldschmidt, J. Chem. Soc. (Resumed) (1937) 655 (https://doi.org/10.1039/JR9370000655) 5. M. Bernat, Cah. ORSTOM Ser. Geol 7 (1975) 65 (https://core.ac.uk/download/pdf/39881849.pdf) 6. V. Zepf ...Zlatko Nikolovski, Jelena Isailović, Dejan Jeremić, Sabina Kovač, Ilija Brčeski. "Some examples of interactions between certain rare earth elements and soil" in Journal of the Serbian Chemical Society, National Library of Serbia (2021). https://doi.org/10.2298/JSC211006095N
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Hidrogeoekološki aspekti aksploatacije uglja u Pelagonijskom basenu (Makedonija)
Kostadin J. JOVANOV (2016)Kostadin J. JOVANOV. Hidrogeoekološki aspekti aksploatacije uglja u Pelagonijskom basenu (Makedonija), Beograd:Rudarsko Geološki Fakultet, 2016
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Kinetics, mechanism, and equilibrium studies of the reactions between a ruthenium(II) complex and some nitrogen- and sulfur-donor nucleophiles
Aleksandar M. Mijatović, Ratomir M. Jelić, Jovana Bogojeski, Živadin D. Bugarčić, Biljana Petrović (2013)Kinetika i mehanizam reakcija supstitucije između [Ru(trpi)(bpi)Cl]+ sa nukleofilima gvanozin-5′-monofosfatom, L-histidinom, tioureom i dimetilsulfoksidom proučavani su spektrofotometrijski u 0,1 M NaClO4 na 310 K. Red reaktivnosti za odabrane ligande je: tiourea > gvanozin-5′-monofosfat > L-histidin > DMSO. Ovaj red je povezan sa elektronskim, strukturnim i hemijskim karakteristikama kompleksa i nukleofila. Reakcija supstitucije sa tioureom je proučavana na tri različite temperature (288, 298 i 310 K). Negativna entropija aktivacije DS = potvrđuje asocijativni način aktivacije. Formiranje kompleksa [Ru(trpi)(bpi)H2O]2+ sa ligandima ...... V, Serli B, Iengo E, Alessio E, Mestroni G (2002) Eur J Cancer 38:427 28. Corral E, Hotze ACG, den Dulk H, Leczkowska A, Rodger A, Hannon MJ, Reedijk J (2009) J Biol Inorg Chem 14:439 29. Kobayashi K, Ohtsu H, Wada T, Kato T, Tanaka K (2003) J Amer Chem Soc 125:6729 30. Chanda N, Mobin SM, Puranik ...
... Moucheron C (2009) New J Chem 33:235 9. Ronconi L, Sadler PJ (2007) Coord Chem Rev 251:1633 10. Jakupec MA, Galanski M, Arion VB, Hartinger CG, Kepplere BK (2008) Dalton Trans 183 11. Durig JR, Danneman J, Behnke WD, Mercer EE (1976) Chem Biol Interact 13:287 12. Novakova O, Kasparkova J, Vrana O, Vanvliet ...
... Vanvliet PM, Reedijk J, Brabec V (1995) Biochemistry 34:12369 13. Vanvliet PM, Toekimin SMS, Haasnoot JG, Reedijk J, Novakova O, Vrana O, Brabec V (1995) Inorg Chim Acta 231:57 14. Vilaplana R, Romero M, Quiros M, Salas J, Gonzalez-Vilches F (1995) Met-Based Drugs 2:211 15. Chatterjee D, Mitra A, De ...Aleksandar M. Mijatović, Ratomir M. Jelić, Jovana Bogojeski, Živadin D. Bugarčić, Biljana Petrović. "Kinetics, mechanism, and equilibrium studies of the reactions between a ruthenium(II) complex and some nitrogen- and sulfur-donor nucleophiles" in Monatshefte für Chemie - Chemical Monthly, Springer Science and Business Media LLC (2013). https://doi.org/10.1007/s00706-013-1044-1
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Application of the VIKOR Method for Selecting the Purpose of Recultivated Terrain after the End of Coal Mining
Radmila Gaćina, Sanja Bajić, Bojan Dimitrijević, Tomislav Šubaranović, Čedomir Beljić, Dragoljub Bajić (2024)Radmila Gaćina, Sanja Bajić, Bojan Dimitrijević, Tomislav Šubaranović, Čedomir Beljić, Dragoljub Bajić. "Application of the VIKOR Method for Selecting the Purpose of Recultivated Terrain after the End of Coal Mining" in Proceedings of the Bulgarian Academy of Sciences, Bulgaria, 28. maj 2024 , Prof. Marin Drinov Publishing House of BAS (Bulgarian Academy of Sciences) (2024). https://doi.org/10.7546/CRABS.2024.07.10
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A contribution to the knowledge of facial diversity of Badenian sediments in the Belgrade area
Filip Anđelković, Dejan Radivojević (2018)... Anđelković, J., 1997. Badenski ciklusi u Srbiji. Geološki anali Balkanskog poluostrva, 61 (2), 1–13. Gruber, B., 1988. Mineraliensammlung E. W. Ricek. Oberösterreichischer Musealverein – Gesellschaft für Landeskunde, 80–110. 236 Marović, M., Toljić, M., Rundić, Lj., Milivojević, J., 2007. N ...
... facija: tašmajdanski krečnjaci, rakovički peskovi, višnjičke gline, konjarnički pteropodski šlir (Anđelković, M., 1987; Anđelković M. & An‐ đelković J., 1997). U dosadašnjim interpretacijama postoje izvesne razlike, bilo u geografskom raspro‐ stranjenju, bilo u samoj odredbi starosti ...
... Na slici 1 prikazana je paleogeografsko‐facijalna karta sa rasprostranjenjem facija prema Stevanoviću (1974). Anđelković M. i Anđelković J. (1997) su u svom radu badenske sedimente Srbije podelili u dva ciklusa sedimentacije, gornji i donji. Prema njihovom shvatanju, facije tašmajdanski ...Filip Anđelković, Dejan Radivojević. "A contribution to the knowledge of facial diversity of Badenian sediments in the Belgrade area" in 17th Serbian Geological Congress, Vrnjačka Banja, 17-20 maj 2018, Srpsko geološko društvo (2018)
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Model za određivanje efikasnosti odvodnjavanja bunarima na primeru površinskog kopa «Drmno»
Anđica J. Kričković (2003)Anđica J. Kričković. Model za određivanje efikasnosti odvodnjavanja bunarima na primeru površinskog kopa «Drmno», Beograd:Rudarsko-geološki fakultet, 2003
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The influence of Al<sup>3+</sup>ion on porcine pepsin activity<i>in vitro</i>
The in vitro effect of Al3þ ions in the concentration range 1.7·1026M–8.7·1023M on pepsin activity at pH 2, via kinetic parameters and its electrophoretic mobility was evaluated. Kinetic study demonstrated the existence of an activation effect of Al3þ at pH 2 on pepsin molecule. Kinetic analysis with respect to concentrations of haemoglobin showed that Al3þ ions increase the maximal velocity (Vmax) and kcat values rather than apparent affinity for substrate (KS) implying the non-competitive nature of activation which indicated ...... of endothiapepsin. J Mol Biol 1990;211:919—0941. 5] Pedersen VB, Foltmann B. The amino acid sequence of a hitherto unobserved segment from porcine pepsinogen preceding the N-terminus of pepsin. FEBS Lett 1973; 35:250—258. 6] Sepulveda P, Marciniszyn J, Lui D, Tang J. Primary structure of ...
... performed in triplicate. RIGHTSLIMKMK&~Ž --| zj g s P o 5 | Š o S - s = 5 j| E > F3 E o 9 Š Đ 8 8 -| = P F-| |- o al Ch em is tr y Do wn lo ad ed fr om -| -} P |l = & Š |-5} |j 6 | || F| 5 -i Fo r pe rs on al us e on ly . in dose-dependent manner ...
... concentrations at pH2. RIGHTSLIMKMK&~Ž --| zj g s P o 5 | Š o S - s = 5 j| E > F3 E o 9 Š Đ 8 8 -| = P F-| |- o al Ch em is tr y Do wn lo ad ed fr om -| -} P |l = & Š |-5} |j 6 | || F| 5 -i Fo r pe rs on al us e on ly . 1006 I7 M. Pavelhic et al ...Vesna M. Pavelkić, Kristina R. Gopcević, Danijela Z. Krstić, Marija A. Ilić. "The influence of Al3+ion on porcine pepsin activityin vitro" in Journal of Enzyme Inhibition and Medicinal Chemistry, Informa UK Limited (2008). https://doi.org/10.1080/14756360701841095
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Kristalografsko ispitivanje nefelinskih i karnegitskih faza dobijenih postupkom termalne transformacije sintetičkih zeolita
Predrag J. Vulić (2005)Predrag J. Vulić. Kristalografsko ispitivanje nefelinskih i karnegitskih faza dobijenih postupkom termalne transformacije sintetičkih zeolita, Beograd:Rudarsko-geološki fakultet, 2005
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Fizičko-geografske karakteristike vulkana Teide na Kanarskim ostrvima
Radovanović D., Srećković -Batoćanin D., Valjarević A., Ivanović R., Veselinović J.. "Fizičko-geografske karakteristike vulkana Teide na Kanarskim ostrvima" in 4. Srpski Kongres geografa, Kopaonik 7-9.oktobar (2015)
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Razvoj metodologije zaštite izvorišta podzemnih voda primenom karata ranjivosti
Vladimir J. ŽIVANOVIĆ (2016)zaštita podzemnih voda, izvorište podzemnih voda, zone sanitarne zaštite, TDM metoda, kretanje podzemnih vodaVladimir J. ŽIVANOVIĆ. Razvoj metodologije zaštite izvorišta podzemnih voda primenom karata ranjivosti, Beograd:Rudarsko Geološki Fakultet, 2016
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Formaciono-mineragenetska analiza karbonatnih sedimenata Jadransko-jonske zone Crne Gore kao sirovinske baze ukrasnog građevinskog kamena
Dragan J. Ilić (2004)Dragan J. Ilić. Formaciono-mineragenetska analiza karbonatnih sedimenata Jadransko-jonske zone Crne Gore kao sirovinske baze ukrasnog građevinskog kamena, Beograd:Rudarsko-geološki fakultet, 2004
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Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation
kontinentalna tektonika: kompresija, kontinentalna tektonika: ekstenzija, kontinentalna tektonika: transkurentni i transformni rasedi, pukotine, rasedi, zone snažnih deformacija, kinematika deformacija kore i omotača, teorijska mehanika, modelovanje... tensor B. The components of finite strain tensors E and E∗ read (Malvern 1969): Ei j = 1 2 ( ∂ui ∂ X j + ∂u j ∂ X i + ∂uk ∂ X i ∂uk ∂ X j ) (25) E∗ i j = 1 2 ( ∂ui ∂x j + ∂u j ∂xi − ∂uk ∂xi ∂uk ∂x j ) . (26) The Lagrange–Green strain tensor contains partial derivatives with respect ...
... deformation in laboratory models, J. geophys. Res., 121(4), 2852–2872. Gomes, A., Rosas, F., Duarte, J., Schellart, W., Almeida, J., Tomás, R. & Strak, V., 2019. Analogue modelling of brittle shear zone propagation across upper crustal morpho-rheological heterogeneities, J. Struct. Geol., 126, 175–197 ...
... application to subduction experiments, J. Geodyn., 100, 7–32. Searle, M.P., Elliott, J., Phillips, R. & Chung, S.-L., 2011. Crustal– lithospheric structure and continental extrusion of Tibet, J. Geol. Soc., 168(3), 633–672. Senatore, C., Wulfmeier, M., Vlahinić, I., rade, J. & Iagnemma, K., 2013. De- sign ...Taco Broerse, Nemanja Krstekanić, Cor Kasbergen, Ernst Willingshofer. "Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation" in Geophysical Journal International, Oxford University Press (OUP) (2021). https://doi.org/10.1093/gji/ggab120
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Selection of Artificial Lift Methods: A Brief Review and New Model Based on Fuzzy Logic
Miroslav Crnogorac, Miloš Tanasijević, Dušan Danilović, Vesna Karović Maričić, Branko Leković (2020)Artificial lift methods have applications in oil wells where oil production is no longer possible due to natural reservoir energy, so this necessary energy is added by introducing lift methods. In order to achieve optimum production, the selection of an artificial lift method is very important. This paper uses fuzzy logic as a mathematical and conceptual model for selection of the optimal artificial lift method. The outcome or IF-THEN rules, as the central part of the model, is based ...... . , µA j, . . . , µA n); B = (µB 1, . . . , µB j, . . . , µB n); C = (µC 1, . . . , µC j, . . . , µC n); (2) M assessment is obtained in the form: µM = (MAXj=1, . . . , MAXj=10) = (µM 1, . . . , µM 10) where: MAXj = max{MINo}, for every j and MINo = min{µA j = 1, . . . , 10, µB j = 1, . . ...
... In dependence of μ, fuzzy number (FN) can be presented in form (1): FN = (μ j = 1, … μ j = 10) (1) Linguistic variables (H) can be presented in the same form. For example, if H = Very low, μ = 1 for j = 1, 2; μ = 0 for j = 3, ..., 10. Other fuzzy sets can be written as: low = (0/1, 0/2, 1/3, 1/4 ...
... In dependence of µ, fuzzy number (FN) can be presented in form (1): FN = (µ j = 1, . . . µ j = 10) (1) Linguistic variables (H) can be presented in the same form. For example, if H = Very low, µ = 1 for j = 1, 2; µ = 0 for j = 3, ..., 10. Other fuzzy sets can be written as: low = (0/1, 0/2, 1/3, 1/4 ...Miroslav Crnogorac, Miloš Tanasijević, Dušan Danilović, Vesna Karović Maričić, Branko Leković. "Selection of Artificial Lift Methods: A Brief Review and New Model Based on Fuzzy Logic" in Energies, MDPI AG (2020)
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The Potential of Biomarkers to Distinguish Lower and Middle Miocene Lignites from the Coal-Mining District of Lusatia
... of Lusatia I. Kojic, J. Kus, D. Zivotic, K. Stojanovic Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] The Potential of Biomarkers to Distinguish Lower and Middle Miocene Lignites from the Coal-Mining District of Lusatia | I. Kojic, J. Kus, D. Zivotic, K. ...
... Montpellier, France THE POTENTIAL OF BIOMARKERS TO DISTINGUISH LOWER AND MIDDLE MIOCENE LIGNITES FROM THE COAL-MINING DISTRICT OF LUSATIA I. Kojić1, J. Kus2, D. Životić1, K. Stojanović1 1University of Belgrade, Serbia 2Federal Institute for Geosciences and Natural Resources, Germany The organic ...
... References Bechtel, A., Sachsenhofer, R.F., Markic, M., Gratzer, R., Lücke, A., Püttmann, W., 2003. Organic Geochemistry 34, 1277–1298. Kus, J., Dolezych, M., Schneider, W., Hofmann, T., Visiné Rajczi, E., 2020. International Journal of Coal Geology 217, 103283. Nytoft, H.P., Kildahl-Andersen ...I. Kojic, J. Kus, D. Zivotic, K. Stojanovic. "The Potential of Biomarkers to Distinguish Lower and Middle Miocene Lignites from the Coal-Mining District of Lusatia" in 30th International Meeting on Organic Geochemistry (IMOG 2021), European Association of Geoscientists & Engineers (2021). https://doi.org/10.3997/2214-4609.202134092
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Comprehensive Profiling of Microbiologically Induced CaCO3 Precipitation by Ureolytic Bacillus Isolates from Alkaline Soils
Olja Šovljanski, Lato Pezo, Jovana Stanojev, Branimir Bajac, Sabina Kovač, Elvira Tóth, Ivan Ristić, Ana Tomić, Aleksandra Ranitović, Dragoljub Cvetković, Siniša Markov (2021)MICP process, kinetic study, calcite, vaterite, MALDI-TOF identification, Bacillus licheniformis, Sporosarcina pasteurii... Arctic seawater. PLoS ONE 2007, 12, e0181860. [CrossRef] [PubMed] 38. Guo, L.; Ye, L.; Zhao, Q.; Ma, Y.; Yang, J.; Luo, J. Comparative study of MALDI-TOF MS and VITEK 2 in bacteria identification. J. Thorac. Dis. 2014, 6, 534–538. 39. Abdel Samad, R.; Al Disi, Z.; Mohammad Ashfaq, M.Y.; Wahib, S.M.; Zouari ...
... rice under saline conditions. J. Plant. Inter. 2014, 9, 379–387. [CrossRef] 42. Orhan, F.; Gulluce, M. Isolation and characterization of salt-tolerant bacterial strains in salt-affected soils of erzurum, Turkey. Geomicrobiol. J. 2014, 32, 521–529. [CrossRef] 43. Zhang, J.; Xie, L.; Huang, X.; Liang, ...
... tion of stone monuments a worldwide issue. Open Conf. Proc. J. 2016, 7, 29–38. [CrossRef] 6. Tiano, P.; Biagiotti, L.; Mastromei, G. Bacterial bio-mediated calcite precipitation for monumental stones conservation: Methods of evaluation. J. Microbiol. Meth. 2019, 36, 139–145. [CrossRef] 7. Ersan, Y.; ...Olja Šovljanski, Lato Pezo, Jovana Stanojev, Branimir Bajac, Sabina Kovač, Elvira Tóth, Ivan Ristić, Ana Tomić, Aleksandra Ranitović, Dragoljub Cvetković, Siniša Markov. "Comprehensive Profiling of Microbiologically Induced CaCO3 Precipitation by Ureolytic Bacillus Isolates from Alkaline Soils" in Microorganisms, MDPI AG (2021). https://doi.org/10.3390/microorganisms9081691
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Natural two-dimensional pyrophyllite: Nanoscale lubricant, electrical insulator and easily-machinable material
Borislav Vasić, Radoš Gajić, Ivana Milošević, Žarko Medić, Marina Blagojev, Marko Opačić, Aleksandar Kremenović, Dejan Lazić (2022)Pyrophyllite, with the chemical formula Al2Si4O10(OH)2, is a naturally occurring and abundant van der Waals mineral belonging to the group of phyllosilicates. It is very soft, layered crystal used for sculpting and an excellent electrical and thermal insulator aimed for the operation at high pressure and temperature. Here, for the first time, two-dimensional (2D) pyrophyllite obtained by both mechanical and liquid phase exfoliation is presented and investigated at the nanoscale. The layered structure provides low friction coefficient of around ...Atomic force microscopy, Insulating properties, Nanofriction and wear, Natural two dimensional materials, Phyllosilicates, PyrophylliteBorislav Vasić, Radoš Gajić, Ivana Milošević, Žarko Medić, Marina Blagojev, Marko Opačić, Aleksandar Kremenović, Dejan Lazić. "Natural two-dimensional pyrophyllite: Nanoscale lubricant, electrical insulator and easily-machinable material" in Applied Surface Science, Elsevier BV (2022). https://doi.org/10.1016/j.apsusc.2022.155114
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Direct selective lead, copper and zinc minerals flotation from polymetallic ore “Podvirovi”
Lazić Predrag, Vučinić Dušica, Stanojev J., Micović B.. "Direct selective lead, copper and zinc minerals flotation from polymetallic ore “Podvirovi”" in Journal of Mining Science 46 no. 6, :Elsevier (2010): 690-694