Претрага
684 items
-
Preliminary regional landslide susceptibility assessment using limited data
Igor Peshevski, Milorad Jovanovski, Biljana Abolmasov, Jovan Papic, Uroš Đurić, Miloš Marjanović, Ubydul Haque, Natasha Nedelkovska (2019)In this paper a heuristic approach for preliminary regional landslide susceptibility assessment using limited amount of data is presented. It is called arbitrary polynomial method and takes into account 5 landslide conditioning parameters: lithology, slope inclination, average annual rainfall, land use and maximum expected seismic intensity. According to the method, in the first stage, a gradation is performed for each of the carefully selected conditioning parameters by assigning so called rating points to the grid cells on which the ...... 10.1007/s12665-010-0724-y COROMINAS, J., VAN WESTEN, C., FRATTINI, P., CASCINI, L., MALET, J-P., FOTOPOULOU, S., CATANI, F., VAN DEN EECKHAUT, M., MAVROULI, O., AGLIARDI, F., PITILAKIS, K., WINTER, M.G., PASTOR, M., FERLISI, S., TOFANI, V., HERVAS, J. & SMITH, J. T. (2014): Recommendations for the ...
... POMAROLI, G., PROSKE, H. & SCHWEIGL, J. (2012): Land- slide susceptibility maps for lower Austria, methods and challenges.– In: Proceed- ings of 12th Congress INTERPRAEVENT 2012, Grenoble, France, 497–508. GÜNTHER, A., EECKHAUT, M., REICHENBACH, P., HERVÁS, J., MALET, J.P., FOSTER, C. & GUZZETTI ...
... SILVA, P. F., ANDERSEN, P., PILZ, J., R. CHALOV, S., MALET, J.P., JEMEC AUFLIČ, M., ANDRES, N., POYIADJI, E., LA- MAS, P.C., ZHANG, W., PESHEVSKI, I., G. PÉTURSSON, H., KURT, T., DOBREV, N., GARCÍA-DAVALILLO, J.C., HALKIA, M., FERRI, S., GA- PRINDASHVILI, G., ENGSTRÖM, J. & KEELLINGS, D. (2016): Fatal ...Igor Peshevski, Milorad Jovanovski, Biljana Abolmasov, Jovan Papic, Uroš Đurić, Miloš Marjanović, Ubydul Haque, Natasha Nedelkovska. "Preliminary regional landslide susceptibility assessment using limited data" in Geologica Croatica , Croatian Geological Society (2019). https://doi.org/10.4154/gc.2019.03
-
Geochemical characterization of sediments from the archaeological site Vinča – Belo Brdo, Serbia
Gorica Veselinović, Dragana Životić, Kristina Penezić, Milica Kašanin-Grubin, Nevenka Mijatović, Jovana Malbašić, Aleksandra Šajnović (2020)Gorica Veselinović, Dragana Životić, Kristina Penezić, Milica Kašanin-Grubin, Nevenka Mijatović, Jovana Malbašić, Aleksandra Šajnović. "Geochemical characterization of sediments from the archaeological site Vinča – Belo Brdo, Serbia" in CATENA, Elsevier BV (2020). https://doi.org/10.1016/j.catena.2020.104914
-
State and perspective of individual household heating in Serbia: A survey-based study
This paper presents the results of the household survey on individual household heating systems in Serbia. The survey was conducted in the period October to December 2020 with the participation of 1100 households with individual household heating systems. The information collected in the questionnaire can be separated into three main parts: basic household data, current heating system characteristics, and households’ perceptions and attitudes. The survey results provide unique and comprehensive information concerning individual household heating systems and the main ...Boban Pavlović, Dejan Ivezić, Marija Živković. "State and perspective of individual household heating in Serbia: A survey-based study" in Energy and Buildings, Elsevier BV (2021). https://doi.org/10.1016/j.enbuild.2021.111128
-
Анализа специфичних услова циркулације карстних подземних вода врела Градишта
Јована Јанковић (2024)Карстно врело „Градиште“ налази се у истоименом селу, и користи се у сврху водоснабдевања града Пирота и околних села. Врело је настало на контакту неогених творевина Пиротске котлине и карстног масива Старе планине. Карстна издан сама по себи је хетерогена и анизотропна те се тешко успостављају правила и принципи циркулације подземних вода. О специфичности циркулације предметног врела најбоље говори анализа изотопске методе где је добијена старост воде и установљено постојање полумладих вода које залежу дубље у односу на младе ...... NM - ceeeposanao, b – 0pauna eempa, 1 — uecmuHa gempa,(npeyaemo o0 Munanosauh & Ifempoauh, 2022) Mep N NE E SE s SW / NW r b U Bb U b U b J b J b J b J b u 1991 15 4 U 5 2,8 2 233 123 l4 I2 28 9 29 7 23 142 1992 16 34 2 10 1ı,9 2 82 5 #8 3 6 36 90 2, 3107 1993 17 3 2ž23 # 2,1 8 22 9L 24 22 ...
... 0. Toyne (1883), J. OKyjonha (1883), T. BoRuepa (1903, 1907), I. JaRKoBuha H npyrax ayropa. MnnBaja ce 9KyjoBuhenBa „I paba a3a reonmorujy JyroucrouHe CpOnje” Kao paji KojH je Ouo nojutora naJjbHM HcCTpa;xkKHBaMbHMa. /[ortpHHOc O IO3HaBaMby TCOJIOTHje OBHX TepcHa laH cy J. Innjah (1924, 1926) ...
... IIpor, VJIK: 551.528 . IlerpoBuh J., 1976: Jave a nehaHe CP Cponje, BojnoH3naBaukH 3aBOJL, Beorpajn, m. 512 IIonmomuuh /I1., Bacgh Jb., ManagHopBuHh C., IIerpoBaHh B., Pacrah Bakamatm 5., Bacah Jb., MapHHonpBuh B., Bajah /I, XajnaH B., dokopuno MnmHh M., Parkonh J., 2021: OJpD:;KHBO yIpaBJbabe ...Јована Јанковић. Анализа специфичних услова циркулације карстних подземних вода врела Градишта, 2024
-
Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia
This paper presents LA-ICP-MS data for garnets from the Rudnik skarn deposit (Serbia), which range from Grs45–58Adr40–52Alm2–3 in the core and Adr70–97Grs2–29Sps1 in the rim displaying anisotropy and zoning. In spite of wide compositional variations the garnets near the end-member of andradite (Adr > 90) are generally isotropic. Fe-rich rims exhibit LREE depletion and flat HREE pattern with weak negative Eu anomaly, including higher As and W contents. On the other side, the Fe-poorer core shows flat REE pattern ...... garnet from the Weondong W-skarn deposit, South Korea. Chemical Geology 451, 135–153. https://doi.org/10.1016/j. chemgeo.2017.01.011 Paton C., Hellstrom J., Paul B., Woodhead J. & Hergt J. 2011: Iolite: Freeware for the visualization and processing of mass spectro- metric data. Journal of Analytical ...
... 251–259. https://doi.org/10.1127/ejm/10/2/0251 Pamić J. & Šparica M. 1983: The age of the volcanic of Požeška Gora (Croatia, Yugoslavia). Radovi Jugoslovenske Akademije Zna nosti i Umjetnosti 404, 183–198. Park C., Song Y., Kang I., Shim J., Chung D. & Park C. 2017: Metaso- matic changes during ...
... indicator of infil- tration metasomatism. Mineralogical Magazine 55, 357–365. https://doi.org/10.1180/MINMAG.1991.055.380.06 Zhai D., Liu J., Zhang H., Wang J., Su L., Yang X. & Wu S. 2014: Origin of oscillatory zoned garnets from the Xieertala Fe–Zn skarn deposit, northern China: In situ LA–ICP-MS ...Bojan Kostić, Danica Srećković-Batoćanin, Petyo Filipov, Pavle Tančić, Kristijan Sokol. "Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia" in Geologica Carpathica, Central Library of the Slovak Academy of Sciences (2021). https://doi.org/10.31577/GeolCarp.72.1.2
-
Петрологија црвених пешчара источне Србијe
Андреј Марковић (2024)У источној Србији формација црвених пешчара има велико распрострањење и улази у састав многих планина овог дела наше земље. Формацију чине кластичне стене интензивно црвене боје псамитске, ређе псамитско-псефитске структуре и алевритске структуре. Ове стене леже трансгресивно преко старијих пермо-карбонских и карбонских стена, док навише прелазе у доњотријаске седименте. Формација црвених пешчара захвата два појаса унутар Карпато-балканида – унутрашњи и средишњи део. Узорци анализирани у овом раду део су средишњег појаса. Тема завршног рада је петрологија црвених пешчара источне ...... š izvor HOTEL _ = — / ii Sv.Petka 'KOLIBA" d —. -—;__ ~ K, jutnica - – e= — MNJ -, VOGOXEN Me / - Š d ) J —jječar ·. o » u ~ . KPATyJEBAL N • E Z Caee – o e ž PAREBO. - e e a j \Niš -a KPyUJEBAU — Ć — A | OB EO -A NI ~ e -) u ap KGcCeCXA | _neECKOBALA) „ - OOO — a a _Sa _ - ...
... VHHBep3aHMTeT y Beorpay — Pyjnapcko- TCOJIOIHKH (baKyJITCT. – Cvijić J. (1924): Geomorfologija, knj. I, Beograd. 21 Obopasay 1 H3JABA O AVYTOPCTBY 3ABPIIHOT PAJIA MMe H IIpe3HMe cTyJIeHTa Al*\gpšj H L KO'@\VH] Bpoj BHJieKca PM j 41' HysjaBMmbyjeM Ja je 3aBpmiHH paji 0J1 HaCJIOBOM {l Teoc10(u ...
... Beorpa/ ZlaryM ojr0pane: PE3HME V ucrouHoj CpOMjI „wdopMamuwja npBeHMx memuapa MMa BeJMKO pacnpocrpabeme H yJa3H y CaCTaB MHOTMX IIIaHHHa OBOT J(eMa HaIC 3CMJbC. OopManujy uHHC KJaCTHUHC CTCHC HHTCH3HBHO IIpBeHe Ooje HcaMMTcCKe, pebe TICAMHTCKO-HCe(DHTCKC CTpyKType H aJeBDHTCKe CTpyKType. OB ...Андреј Марковић. Петрологија црвених пешчара источне Србијe, 2024
-
Hypogene speleogenesis related to porphyry magmatic intrusions and its influence on subsequent karst evolution in the Peruvian high Andes
Alexander Klimchouk, David Evans, Sasa Milanovic, Cristian Bittencourt, Mauro Sanchez, F. Carlos Aguirre (2022)Alexander Klimchouk, David Evans, Sasa Milanovic, Cristian Bittencourt, Mauro Sanchez, F. Carlos Aguirre. "Hypogene speleogenesis related to porphyry magmatic intrusions and its influence on subsequent karst evolution in the Peruvian high Andes" in Geomorphology, Elsevier BV (2022). https://doi.org/10.1016/j.geomorph.2022.108488
-
Lower Berriasian ammonites from Dedina (Golubac Mountains, eastern Serbia) and their biostratigraphic implication
... |_f|4 Hi LI | |}- -} -_-L}] E B I J EsH|I ||BLJ-| a -B EaE E s |M | LJ |E | J E || || || A / | | j ||> |M | || }A | | || -i I L J Lj - I - - -| | - { | LJ ||_|| |A|}_| |_{L_| |f= | L J i |Epi|s | s | | 5 / % Bie|||s|P|P{E|S| ...
... seje2oouanojsqns ___ee- snjejnojossj sojtuejdqnsopnescj —___e- IJouoj s e j u u e J j d q n s o p n o s c e e e — - Jedse '}o SeJeO!SOqJE}/ • uunojojd '} SeJaolJeJ5aN • s n o n u o d ·}o s e j i u p / d q n s o p n e s c ___ __e-– _ – I I uunujuu SeJeoiJeuBeN- ...
... 'ds sejiue/u00g — e- "An{ ·ds sojjueluDog. uunuuos!oj sejeoossijod/}H u i n u b 9 J o J 5 o p n e s d sejeoljidS SIsuejeABuhu; BjjeuludjeQ ___e- sisueutudjep '}o Bjjeuiudjeg uejuouqns sejuueJdqnsopnescj uunjeuulje SeJe20JdB}- • sipue-56 sejjuejdqnsopnes, PojujjedJeD ...Zdenek Vasícek , Dragoman Rabrenović, Petr Skupien, Barbara Radulović. "Lower Berriasian ammonites from Dedina (Golubac Mountains, eastern Serbia) and their biostratigraphic implication" in Cretaceous Research (2023). https://doi.org/10.1016/j.cretres.2023.105623
-
Application of ERT in the study of debris-flow source area: Case study Selanac debris flow
Dragana Đurić, Jelka Krušić, Biljana Abolmasov. "Application of ERT in the study of debris-flow source area: Case study Selanac debris flow" in 11th Congress of the Balkan Geophysical Society, Volume 2021, Online-Romania, 10 -14. Oct 2021,, European Association of Geoscientists & Engineers (2021). https://doi.org/10.3997/2214-4609.202149BGS15
-
Phase relations and physical indicators of municipal waste from old landfills in Serbia
Due to certain similarities of municipal waste and soil, usually for the determination of basic parameters of physical state, laboratory and field tests which are common in geotechnical investigations are used. It is often to construct an apparatus for special purpose to perform some specific laboratory and field tests. Therefore, different values of indicators of municipal waste physical state can be found in the literature. The basic reasons should be found in different definitions and methods that researchers use ...municipal waste, moisture content, unit weight, specific gravity, grain size distribution, porosityGeneral Computer Science... + . ' 2 IMO ; ; max. 68 % ' .. ' ;l ' ' ' _ . ' ' kx4] HNRA Č, BB ; 44 [00] ~ ILO ' [00] :-{} FIEI] ' J GwULs.m ! —— : Bu4 ı ' Z o . 5 awt6iw ? OB Bt! ' Šl LJ ' ı ' J INJ . ' ' :l s| |} RR r . , ' ' i R- ~ ~ ' = - HE E ı | Bi — ljl ' i = NH ı | Ri = [00 š ' ' NIJ e= | · ...
... Smederevo steel mill, Serbia. J Knviron Prot Ecol,17(2), 512-522. 2) Rakić D.,Basarić l., Čaki L., Ćorić, S. (2018):Contribution to geotechnical classification of municipal wasteJowrmna!l of” FEnvironmental Geotechnics,DO1:10.1680/jenge.18.00028. 3) Skempton A.W., Petley J. (1970): Ignition loss and ...
... display their change, if the initial conditions are known. beforc h·odcgrudaum'\ , iibeć- air (a) h, biodegradation Ž::·'l AhA FB, w water(v) h, j air(a) f water (v) Fig. 3. Phase system change of municipal waste during, iodegradation (Gourc and Staub, 2010). Values of basic physical parameters ...Dragoslav R Rakić, Irena G Basarić Ikodinović, Jovana M Janković, Tina D Đurić. "Phase relations and physical indicators of municipal waste from old landfills in Serbia" in Japanese Geotechnical Society Special Publication, The Japanese Geotechnical Society (2021). https://doi.org/10.3208/jgssp.v09.cpeg016
-
Geonasleđe Golije i Peštera
Ljiljana V. Grujičić-Tešić (2017-09-01)Sprovedena istraživanja u ovoj studiji obuhvatila su izdvajanje, opis, evaluaciju i valorizaciju objekata geonasleđa u cilju razvoja istraživane oblasti sa stanovišta geonauka, geoturizma i geoekologije. Na izučavanom području objekti geonasleđa su evidentirani, interpretirani, vrednovani i kategorisani, dat je predlog promocije geoobjekata, i na kraju predložena dopuna inventara objekata geonasleđa Srbije.U protekle četiri godine, na kompleksu geotopa Golije i Peštera istražena su geološka svojstva stena (tip stene, starost, fosilni sadržaj, morfološke i hidrogeološke karakteristike itd.), na osnovu čega je bilo ...... 7428961; 4760266, foto J. Kovačević Erozioni oblici reljefa nastali padinskim procesima predstavljeni su brazdama, vododerinama i jarugama. Jaružanje je posebno izraženo u selu Rastanoviće (Slika 31) u čvrstim stenskim masama. Slika 31. Jaružanje u selu Rastanoviće, foto J. Kovačević https://sh ...
... Doktorska disertacilja GEONASLEĐE GOLIJE I PEŠTERA 63 Slika 38. Dostanlik, koordinate 7425564; 4786781, foto J. Kovačević Slika 39. Nemanjića grad, foto J. Kovačević U selu Kumanica nalazi se kameni most preko reke Moravice (Slika 40). Iako nosi ime „Rimski most“, ne pripada ...
... Manastir Studenica, Bogorodičina crkva, foto J. Kovačević http://(www.spomenicikulture.mi.sanu.ac.rs/ Ljiljana V. Grujičić - Tešić Doktorska disertacilja GEONASLEĐE GOLIJE I PEŠTERA 70 Slika 49. Manastir Studenica, kula (pirg), foto J. Kovačević Manastir Studenica (Slika 50) je ...Ljiljana V. Grujičić-Tešić. "Geonasleđe Golije i Peštera" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2017-09-01)
-
A comparison between ARIMA, LSTM, ARIMA-LSTM and SSA for cross-border rail freight traffic forecasting: the case of Alpine-Western Balkan Rail Freight Corridor
Miloš Milenković, Miloš Gligorić, Nebojša Bojović, Zoran Gligorić. "A comparison between ARIMA, LSTM, ARIMA-LSTM and SSA for cross-border rail freight traffic forecasting: the case of Alpine-Western Balkan Rail Freight Corridor" in Transportation Planning and Technology, Informa UK Limited (2023). https://doi.org/10.1080/03081060.2023.2245389
-
Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides
Kristof Porkoláb, Szilvia Kövér, Zsolt Benkó, Gabor Héja, Melinda Fialowski, Balázs Soós, Nataša Gerzina Spajić, Nevenka Đerić, László Fodor (2019)Internal Dinarides, Drina-Ivanjica thrust sheet, Deformation history, K–Ar dating, Obduction, Structural analysis... V., Bernroider, M., & Genser, J. (2014). The origin and age of the metamorphic sole from the Rogozna Mts., Western Vardar Belt: new evidence for the one-ocean model for the Balkan ophiolites. Lithos, 192, 39—55. Spray, J., Bćbien, J., Rex, D., & Roddick, J. (1984). Age constraints on the ...
... Kononkova, N., Simakin, S., Olujić, J., et al. (2009). Mantle peridotites from the Dinaridic ophiolite belt and the Vardar zone western belt, central Balkan: A petrological comparison. Lithos, 708(1), 37—71. Belak, M., Jamičić, D., Crnko, J., & Sremac, J. (1995). Low- metamorphic rocks from ...
... 261—279. Gawlick, H.-J., Frisch, W., Hoxha, L., Dumitrica, P., Krystyn, L., Lein, R., et al. (2008). Mirdita Zone ophiolites and associated sediments in Albania reveal Neotethys Ocean origin. Interna- tional Journal of Earth Sciences, 97(4), 865–881. Gawlick, H.-J., Sudar, M., Suzuki, H., ...Kristof Porkoláb, Szilvia Kövér, Zsolt Benkó, Gabor Héja, Melinda Fialowski, Balázs Soós, Nataša Gerzina Spajić, Nevenka Đerić, László Fodor. "Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides" in Swiss Journal of Geosciences (2019)
-
Analysis of a simplified model for determining rock mass oscillation velocity at the Kovilovača open pit
... ground vibration in rock-soil interface. Jourma! of Rock Mechanics and Geotechnical Engineering 2019, 77(4), pp. 770-778. 2. Feher,J.; Cambal, J.; Pandula, B.; Kondela, J.; Sofranko, M.; Mudarri, T.; Buchla, I. Research of the technical seismicity due to blasting: works in quarries and their impact ...
... Equation (5) can be written in the form: — %* — · R whereby integration, it is obtained: v Av AR — ~-n·| —,,respectively: logv=logR" +logC; j v j R p y: 108 ii Š (6) where C is a constant of integration. Equation (6) can be written in the form: logv=logC·R"; () 4. MODELS FOR DETERMINING ...
... S.; Gluščević, B.; Tokalić, R.; Majstorović, J.; Beljić, Č. Models of Determining the Parameters of Rock Mass Oscillation Equation with Experimental and Mass Blastings. Minerals 2018, &(2), 70. Lutovac, S.; Gluščević, B.; Gligorić, M.; Majstorović, J.; Tokalić, R. Simplified model for determining ...Suzana Lutovac, Miloš Gligorić, Jelena Majstorović, Luka Crnogorac. "Analysis of a simplified model for determining rock mass oscillation velocity at the Kovilovača open pit" in 9th International Conference Mining and Environmental protection MEP, 24 – 27 May 2023, Sokobanja, Serbia, Belgrade : University of Belgrade-Faculty of mining and geology (2023)
-
Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
Finds of Pleistocene rhinoceros are rare in Serbia, and only one species (the woolly rhinoceros Coelodonta antiquitatis Blumenbach, 1799) has been reported so far. The current paper presents the dental material of an extinct so-called Hundsheim rhinoceros, Stephanorhinus hundsheimensis Toula, 1902 from Bogovina Cave (East ern Serbia). Both the morphological and metric characteristics of the teeth are consis tent with the attribution to S. hundsheimensis. Unfortunately, the rhinoceros material originated from an uncertain geological context, so there is no ...... Van der Made, J. 2000. A preliminary note on the rhinos from Bilzingsleben. Praehistoria Thuringica, 4:41-64. Van der Made, J. 2010. The rhinos from the middle Pleistocene of Neumark-Nord (Saxony- Anhalt). Veröffentlichungen des Landesamtes für Archäologie, 62:432-527. Van der Made, J. and Montoya ...
... Serbia) for access to the fossil material. We would also like to thank J. van der Made (Museo Nacional de Ciencias Naturales Madrid, Spain) and N. Cvetković (Regional Museum of Jagodina, Serbia) for their useful sug- gestions and comments, J. Lindal (Department of Anthropology, University of Manitoba, Canada) ...
... benthic δ18O records. Paleoceanography, 20:PA1003. https://doi.org/10.1029/ 2004PA001071 Madurell-Malapeira, J., Minwer-Barakat, R., Alba, D.M., Garcés, M., Gómez, M., Aurell-Garrido, J., Ros-Montoya, S., Moyà-Solà, S., and Berástegui, X. 2010. The Vallparadís section (Terrassa, Iberian Peninsula) ...Predrag Radović, Miloš Radonjić, Emmanuel Billia. "Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia" in Palaeontologia Electronica, Coquina Press (2020). https://doi.org/10.26879/985
-
Upper Miocene depositional environments of the Kikinda-Mokrin High (Serbia)
Saša Ivanišević, Dejan Radivojević (2018)Exploration for oil and gas in mature areas, such as the Pannonian Basin, can benefit from reexamination of old data using more advanced modern workflows that focus on the temporal and spatial aspects of sediment deposition. Specifically, we apply a new environment of deposition model that interprets the Upper Miocene- Pliocene sediments as being deposited in a rapidly filling basin characterized by quick shelf edge progradation from the northwest toward the southeast. Reconstruction of this shelf edge trajectory reveals ...Saša Ivanišević, Dejan Radivojević. "Upper Miocene depositional environments of the Kikinda-Mokrin High (Serbia)" in Interpretation, AAPG SEG (2018). https://doi.org/10.1190/INT-2017-0084.1
-
English for Geology Students. 2
Lidija Beko (2023)... kks .. .. ... .. Part1 Part 2 Part 3 Part1 Part 2 Part 3 • Unit1 • LANDSLIDES ŠOTIEORIMA:TIONI .J BN .0. . .POOPOVIV-K. -f. · -650 . . j OMLON,. Vocabularyg ... ..032 .J - % . . „ye . • « • < }SLayaji- • • -e 15150 2 Reading Comprehension........... a MASS WASTING AND TYPES „ ttt ...
... . SLOPE STABILITY ... ttt ttt Mocabulary_ y. NN al . JMN a M, 2MA do a a -yy „O laJaM-Jja Reading Comprehension...........ca. (rammarispo{(-. .J . :yar-Ja%93 270 y Myaı . D . - a ı- eyala y a -yskt ipixercisesL, d. ...... a d W · -kef Ag • ,,, 5v -P ON 2 . a SOMa. Geological Wonders....... ...
... through Myths..............a.. 148 • Unit6• GEOPHYSICS, SEISMICITY AND PROSPECTING Partl Seismic waves .......... e 152 Mocabulary.7.09...y. ..0A P J R ). .RkM . R .. RMM . da 155 Reading Comprehension...........te. 157 Part2 SEISMIC MONITORING........ttt tt 158 iWocabulary„...g .. i. -M-fyava ...Lidija Beko. English for Geology Students. 2, Belgrade : The Faculty of Mining and Geology, 2023
-
Groundwater resources for drinking water supply in Serbia´s Southeast Pannonian basin
Dušan Polomčić, Bojan Hajdin, Marina Ćuk, Petar Papić, Zoran Stevanović. "Groundwater resources for drinking water supply in Serbia´s Southeast Pannonian basin" in Carpathian Journal of Earth and Environmental Sciences (2014)
-
Procena poroznosti i litologije na osnovu geofizičkih merenja u severoistočnoj Rumuniji
Manja Grifatong (2024)Geofizička karotažna merenja imaju važnu ulogu u određivanju fizičkih i geoloških svojstava delova Zemljine kore. Cilj ovog rada je da se prikaže procena poroznosti i litoloških karakteristika formacije na osnovu rezultata geofizičkih karotažnih merenja. Na osnovu dostupnih podataka izrađeni su dijagrami promene poroznosti sa dubinom i krosplot dijagrami neutronska poroznost – srednja gustina za dve bušotine koje se nalaze na Moldavskoj platformi, u severoistočnoj Rumuniji. Na osnovu ovih dijagrama određene su zone povećane poroznosti i litologija formacija kroz koje ...... radioaktivnost - GR [GAPI] — Srednja gustina – DEN [g/cm*"| 2 24 2.8 0 40 80 120 350 350 ,A j i i T 400 — 400 —j = Zona 1 450 —j 450 — Zona 2 Du bi na || m| 500 —j 500 —j 550 —j 550 —j Zona 3 T T T T T T T T -80 -40 0 40 80 0.4 0.2 0 Sopstveni potencijal - SP [MV] — Neutronska ...
... vrednosti, dok je merena vrednost gustine niska, kao što je prikazano na slici 2. SREDNJA VREDNOST GUSTINE g/emž »> 23 2a - 26| [ O L O G I J A POROZNOST PEŠČARA 35 30% 2%% 20% 12 Uticaj gasa – PPovećana poroznost | | GAS VODA Slika 2. Uticaj prisustva gasa u formaciji na odziv ...
... mogu pouzdano da se razdvoje (Rider, 2002). Poroznost peščara 30% 20 10 Zona « zaglinjenog peska P O R O Z N O S T M E R E N A NA J E Z G R I M A 40 30 20 10 % Vrednosti poroznosti dobijene Neutronskim karotažom Slika 4. Uticaj prisustva gline (šejla) na neutronsku poroznost ...Manja Grifatong. Procena poroznosti i litologije na osnovu geofizičkih merenja u severoistočnoj Rumuniji, 2024
-
Tektonske i litostratigrafske karakteristike šireg područja Grivske (Zapadna Srbija)
Nikola Otašević (2024)U ovom radu predstavljene su osnovne geološke karakteristike šireg područja Grivske. U litostratigrafskom pogledu na ovom prostoru prisutne su paleozojske, mezozojske i kenozojske sedimentne, magmatske i metamorfne stene. Tvorevine karbona su predstavljene semimeta-morfisanim tvorevinama.Tvorevine trijaske starosti su predstavljene slojevitim i masivnim krečnjacima, dok su tvorevine jure predstavljeni produktima ofiolitskog melanža. Takođe, prisutne su i tvorevine senona koje su predstavljene masivnim krečnjacima. U neogenoj sukcesiji dominiraju klastiti miocena, dok su u kvartaru zastupljeni različiti tipovi fluvijalnih, deluvijalnih i deluvijalno-proluvijalnih tvorevina. ...Nikola Otašević. Tektonske i litostratigrafske karakteristike šireg područja Grivske (Zapadna Srbija), 2024