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Упит dcterms_creator_txt:Michael R. Sandy

795 items

  • Revisiting the Early Jurassic (Sinemurian) brachiopod fauna from Smokovac, Montenegro

    Michael R. Sandy, Barbara V. Radulović, Martin Đaković (2021)

  • Дефинисање геотехничких параметара еолских седимената земуснког платоа на основу лабораторијских и теренских SPT испитивања

    Ђорђе Крзман (2024)
    Циљ овог рада је био да се одреде геотехничке караткеристике предметног терена што представља полазну основу за рационално пројектовање и градњу. Истражним бушењем утврђено је да предметни терен изграђују четри лесна хоризонта и три слоја погребене земље до дубине од 22-23 m. Лабораторијским испитивањем добијени су ефективни параметри смичуће чврстоће, где се кохезија најчешће креће између c’=14 и 18 kPa, а угао унутрашњег трења f'= 25 - 30 °. Теренска SPT испитивањем уз коришћење прихваћених корелација у геотехничкој пракси ...
    лес, лабораторија, SPT, корелације, параметри
    ... Tipatva nocxoaira |Loess-ike deposits |Silt, sandy PZi Tipauta Sit Tipatia rninonira |Sit, cla TE RR ES TI C - M AR SH š Š * š [•] ž š 5 |r [ | [ Tipatva nocxoaira |Sit, sandy Tipatniva, |npauuwwacro-necxoara rnaha. |Sit, silty-sandy clay AT yB IA JA TI HO - B AP CK V ...
    ... ·u•:" % KJ ___ G r — — e p a · —— [ARyBVIJARHE HACTATE ((paturja nononea): Tipauiia nocoanra o necax npauuinacr (ML/SM), vrane. |nnacrwuiocna, BonoaaciheHa, jave crauraina, kpra, cna6o 36ujewa, cpe/iyee Ro cnaGo BononponycHa, |crernocwehe Goje. |ALLUVIAL DEPOSITS (food facies): Sandy sili to silty ...
    ... CKVI CEBIMEHTY{- Tipatnie w npauinincro nockoBnTe TnO y Oknvpy KOJAX Ce- npauiwacro-necxoaura r |uanajajy: ABa xopyaora norpeGee aevise ne6reuha 1-2u (Maehy kora 71-73-upko upaeHe Goje |Sit, silty-sandy dlay 75-77-upko xyre Goje), npauuwiacror w npauiMiacro rnuHoBuror cacTaBa, ca aaGojeteia Mn u Fe ...

  • Дефинисање параметра песковитог тла за потребе прорачуна слегања плиткох темеља преко CPTm и CPTu опита

    Александар Јаковљевић (2024)
    Дефинисање меродавних геотехничких параметара тла за потребе прорачуна слегања.(a и носивости)темељног тла један је од главних задатака инжењера геотехнике.Од поузданости ових параметара и последично резултата прорачуна слегања и носивости, директно зависи који ће се тип, врста и димензије темеља као и начин фундирања истог примењивати.Да би се поуздано дефинисали неопходни геотехнички параметри а потом и извели потребни прорачуни слегања, потребно је на првом месту познавање деформабилних карактеристика тла.Подаци о збијености тла могу се добити или лабораторијским испитивањима на претходно ...
    CPT, песак, слегање, параметри, корелације
    ... (Robertson 2010.) naruH cy Ha c 4,5: qt(MPa)|I 38 Silty sand & sandy silt 44 Sand & silty sand 10.1 Silty sand & sandy silt 5.2 Sand & silty sand 8.2 Silty sand & sandy silt 6.2 Sand & silty sand 10.3 Silty sand & sandy silt 7.4 Sand & silty sand 12.7 M B clay 1.3 Sand & silty sand ...
    ... silty sand 3.5 -| Sand & silty sand 4 4 4.5 -| a i Silty sand & sandy silt 5 Sand & silty sand 5 -| - 55 Sand & silty sand Sand & silty sand -| Silty sand & sandy silt 6| 6| Silty sand & sandy silt 6.5-| Silty sand & sandy silt___| 7 ı 7 Sand & silty sand 7.5 -| ~ 8-| — Sand & silty sand ...
    ... Operator: Uknown Depth (m) Elevation:0.00 (m) Sand & silty sand Silty sand & sandy silt Sand & silty sand Silty sand & sandy silt Sand & silty sand Silty sand & sandy silt Sand & silty sand Silty sand & sandy silt Sand & silty sand Clay Sand & silty sand Description qt (MPa)| 3 ...

  • Geotechnical Conditions for Construction of Savski Trg Metro Station as a Part of the Belgrade Metro Line One

    Nemanja Stanic, Dragoslav Rakic, Josip Isek, Slavoljub Simic (2024)
    In order to solve serious traffic congestion in Belgrade, a number of studies regarding the Belgrade Metro construction have been carried out since 1973. However, only in 2019, the routes of the future metro lines 1 and 2 were de-fined as a part of the General Metro Construction Project. The lines are de-signed to intersect at the location of Sava Square, where an interchange met-ro station will be built. It represents a complex geotechnical structure consist-ing of three different ...
    metro station, geotechnical modelling, displacements

  • Correlation Between Dynamic CBR and Compaction and Bearing Capacity of Pavement Foundation Layers

    Milan Bogdanović, Snežana Bogdanović, Dragoslav Rakić, Irena Basarić Ikodinović (2024)
    This paper presents a dynamic California Bearing Ratio (CBRd) device that can be used on a prepared pavement foundation layer to obtain a certain parameter of the tested material in the laboratory and in situ in a direct and fast way. For the selected natural material (gravel), it is shown that the laboratory CBRd can be used to estimate the compaction and bearing capacity, because it correlates well with the parameters of the standard and modifed Proctor compaction tests. ...
    korelacija parametara, donji slojevi saobraćajnica, laboratorijska i terenska ispitivanja, dinamički kalifornijski indeks nosivosti CBRd
    ... presented [5], and the correlations of the parameters of the laboratory dynamic California Bearing Ratio (CBR, ) with the com- paction properties of sandy soil have been reported [4]. Owing to its short duration and ease, CBR, testing using a LWD can become widespread as an alterna- tive to the classic ...
    ... 14688-2:2018 did not indicate significant differences in the grain size distribution, and it was determined that the material is natural mineral soil, sandy gravel (Sa-Gr), and non-plastic, where one grain size or a grain size range (0.1-0.5 mm) predominates, while some intermediate grain sizes are missing ...
    ... J. Test. Eval., 43(5), 028-1036 (2015). D. Kuttah, “Strong correlation between the laboratory dynamic CBR and the compaction characteristics of sandy soil,” Int. J. Geo-Eng., 10(1), 7 (2019). . Zabielska-Adamska and M. ]. Sulewska, “Dynamic CBR as a method of embankment assessment,” Proc. 18% ...

  • Determining the Groundwater Balance and Radius of Influence Using Hydrodynamic Modeling: the Case Study of the Groundwater Source “Šumice” (Kikinda, Serbia)

    Dušan Polomčić, Dragoljub Bajić, Jelena Zarić (2015)
    A groundwater flow model was developed to simulate groundwater extraction from the public water supply source of the City of Kikinda. The hydrodynamic model includes the municipal groundwater source of Kikinda (Šumice and the Jezero Well), but also an extended area where there are groundwater sources that provide water supply to three factories: (MSK, TM and LŽT - Kikinda). Hydrodynamic modeling, based on the numerical method of finite differences will show the groundwater balance of the sources in the ...
    Water supply, Aquifer, Flow, Groundwater regime, Numerical modeling, Particle tracking
    ... sediments. The base of the Quaternary sediments is made up of shallow lacustrine sediments of the Upper Pliocene. They are built of sandy siltstone, gravelly and sandy siltstone, dark gray siltstone and organogenic silty sands. Carbonaceous interbeds and organic matter are regularly present in these ...
    ... of the Würm age. Sedimentological analyses have shown that the riverine and lacustrine sediments were made of sands, silty sands and alevrites (sandy, rarely clayey and gravelly), while the riverine/bog sediments were composed of clay alevrites and alevrite sands with gravel. Additional units ...
    ... impermeable strata. An important characteristic of these layers is the constant alternation of sands, slightly gravelly sands, with loessial clays, sandy clays, and clays (Figure 3). Figure 3 shows a characteristic lateral alternation and thinning of impermeable layers and the water-bearing layer ...

  • 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 ...
    naftna geologija, depozicione sredine, formacije, Panonski basen

  • Petrological and geochemical studies of lignite from the Tamnava West field, Kolubara basin (Serbia)

    Milena Pajić, Reinhard F. Sachsenhofer, Achim Bechtel, Ksenija Stojanović, Vladimir Krstić, Dragana Životić (2021)
    ... was investigated using micropetrography, proximate and ultimate analyses and biomarker proxy. Upper Miocene (Pontian) coal-bearmg strata consist of sandy-clayey sediments with threc coal seams. The twenty four (24) representative samples originating from borehole PE/Pgh-127.5 from the main coal seam ...
    ... Pi Td „ia ONAJ ОШВР. РРА, 2" ž a 5' а • MO. PETROLOGICAL AND GEOCHEMICAL STUDIES OF LIGNITE FROM THE TAMNAVA WEST FIELD, KOLUBARA BASIN (SERBIA) Р и о Milena Pajić!, Reinhard F. Sachsenhofer", Achim BechteF, Ksenija Stojanović”, Vladimir Krstići, Dragana Životić“ ! Zijin Copper, Svetog Save 2 ...

  • Bearing capacity analysis of vertically loaded piles in sandy soil in New Belgrade, Serbia

    Rakić Dragoslav, Ćorić Slobodan, Šušić Nenad (2010)

  • Towards Sustainable Management of Transboundary Hungarian-Serbian Aquifer

    Zoran Stevanović, Peter Kozák, Milojko Lazić, Janos Szanyi, Dušan Polomčić, Balazs Kovács, Jozsef Török, Saša Milanović, Bojan Hajdin, Petar Papić (2011)
    ... impermeable strata. Sandy-gravel sediments represent major aquifer systems. Their thickness varies from less than 10 m up to 50 m, but is generally of the order of 10 to 20 m. The transmissivity coefficient ranges from 10-s to I0 a m2 s 1. The semi- permeable or fu1ly-impermeable sandy clays often disconnect ...
    ... for industrial purposes. In Serbia it is assumed that the current exploitation of the transboundary aquifer is around 2.8m3 s-1, of which 7.2m3s-t are r-rsed by individual industry and farms. Groundwater is also used for irrigation purposes, but to a lesser extent because of rain-fed agriculture and ...
    ... 120000 100000 z* x -7^*, \-,/. Muoooo $) *0000 40000 200uu 20000 660000 480000- EOY *roPooo .l $n) 640000 I czoooo r000 0 *1000 *2000 r c -3000 o 9 -+ooo !) E -5000 -6000 -7000 -8000 *"l,o,Tio 75oooo Figure 4.9.2 Three-dimensional model and general cross section through the study ...

  • Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)

    Ljupko Rundić, Meri Ganić, Slobodan Knežević, Dejan Radivojević, Miloš Radonjić (2019)
    Mt. Avala is located on the southern margin of the Pannonian basin (SPB), a border zone between the uplifted morphostructures of the Dinarides and Carpathian-Balkanides. Similar to the Pannonian basin, tectonostratigraphic evolution of the Mt. Avala area during the last 23 Ma has is characterized by syn- and post-rifting processes as well as tectonic inversion. Here, we present the results of field investigations of the Miocene‒Pliocene dynamics that led to different spatial positions of the same stratigraphic units (e.g. ...
    мио-плиоценска геодинамика, јужни Панонски басен, Авалски и Торлак хорст, Белопоточки трог, Србија
    ... Ervilia dissita EICHWALD (d). Figure 9. The Lower Pannonian sandy marl (a), sandy marls steeply dipping towards the southeast (b). G eo lo g ia C ro a ti ca Geologia Croatica 72/2116 (Fig. 7), an outcrop of the Lower Pannonian sandy marls, seve- ral metres in height and length, was discovered ...
    ... they con- sist of gray silts and sandy marls (N 44°43′11″, E 20°32′15″ – No.11 in Fig. 1). However, they exhibit a yellow-brown colour on the surface (Fig. 11a, b). The lower, older part of the section with a height of 4 m, is composed of brownish to gray, sandy marl (Fig. 11c, d) which contains ...
    ... thick gray silts contain a similar fossil association (large candonids prevailing among the ostracods – Fig. 11e). They are intercalated with gray sandy silts (up to 1m thick) and a thin interlayer of silts (10–20cm) with Lymnocardium zagrabiense (BRUSINA). Besides molluscs, a very abundant ostracod ...

  • Microstructural and magnetic properties of electrospun hematite/cuprospinel composites

    Mira Ristić, Aleksandar Kremenović, Michael Reissner, Željka Petrović, Svetozar Musić (2020)
    Phase composition, microstructural and magnetic properties of electrospun hematite/cuprospinel composites were investigated. Samples were synthesized starting with 0 to 10 mol% of copper relative to iron. The round shape of reference electrospun fbres was preserved upon their heating up to 600 °C in air, whereas at 700 °C hollow substructure was additionally formed. In these reference samples the presence of hematite phase was detected by XRPD. A small amount (traces) of Fe3O4 /γ-Fe2O3 was also found, due to the ...
    Electrical and Electronic Engineering, Condensed Matter Physics, Atomic and Molecular Physics and Optics, Electronic, Optical and Magnetic Materials

  • Groundwater management by riverbank filtration and an infiltration channel, the case of Obrenovac, Serbia

    Dušan Polomčić, Bojan Hajdin, Zoran Stevanović, Dragoljub Bajić, Katarina Hajdin (2013)

  • Stratigraphy and microfossils (radiolarians and planktonic foraminifers) of the Upper Cretaceous (upper Santonian–lower Campanian) Struganik limestone (Western Serbia)

    Liubov G. Bragina, Nikita Yu. Bragin, Ludmila F. Kopayevich, Nevenka Đerić, Nataša Gerzina Spajić (2019)
    Paleontology, Stratigraphy, Ecology, Evolution, Behavior and Systematics

  • New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)

    Nevenka Đerić, Nataša Gerzina (2014)
    Gornja kreda, radiolarije, Jadar blok, zapadni pojas Vardarske zone, zapadna Srbija
    ... BR 1/4 5 |- BR 1/3 41s |- s e 30 j BR 1/2 2– 1- 0 j BR 1/1 Legend marly limestone |)-w|} limestone with chert nodules -_ sandy limestone conglomerate and sandstone position of radiolarian samples Figure 4:A Generalized columnar section of the Cretaceousin the studied area ...
    ... et al. (1978), Turonian sediments arc represented by detrital limestone with marlstonc interlayers, reddish bedded silicified limestone, marly-sandy conglomeratic limestone and reddish marly claystone. Senonian sedimcnts are best exposed in Stru- ganik village. Thcy are represented by a sequence ...
    ... 14-17, 26-28 are from Sample BR 1/3. Scale bar length for images 1-4, 7-24, 26-30 is 50um; for images 5, 6, 25 is 100nm. Geologia Croatica 67/3 r č| F3 |E -i | s s|s = LNKOS s|s žš|a& Hi F| t [} = s lo ME 5 fj FH s Fj s|m El 5 F| s [5] r3 - |H s E 20 s & Š s s < šŠ Age ...

  • The Rift Sequence Stratigraphy of the Itebej Field (Pannonian Basin, Serbia)

    Saša Ivanišević, Jelena Radišić, Ivana Isić, Dejan Radivojević (2019)
    ... tract sediments which include reef limestones, sandy limestones (rarely) and coarse carbonate sandstones deposited during the Early Badenian Age. Above these shallow marine sediments, the Early Badenian pelagic deeper-water sediments with marls, sandy marls and marly limestones were deposited. The ...

  • Еоценска фауна југозападног дела Сирт басена (Либија)

    Љупко Рундић, Мери Ганић (2020)
    Еоцен, крупни мекушци, нумулити, ЈЗ Сирт басен, Либија

  • Sexual dimorphism and left-right asymmetry of carapace ornamentation in Hemicytheria setosa RUNDIĆ 2002

    Vukica Vujić, Ljupko Rundić, Tamara Karan-Žnidaršič (2019)
    In biostratigraphic research of the Upper Miocene of the Pannonian Basin System, one of the frequently detected and important ostracod genera is Hemicytheria. Among more than 20 species of this genus, Hemicytheria setosa is present in sandy facies of the Lake Pannon sediments in Serbia and Bosnia and Herzegovina. The aims of this study were to describe sexual dimorphism and differences between left and right valve morphology in Hemicytheria setosa. Landmark based geometric morphometrics is applied on the grounds ...
    Morfologija ljušture, Ostrakode, geometrijska morfometrija, gornji miocen, južni deo Panonskog basena

  • Cyanobacterial diversity and toxicity of biocrusts from the Caspian Lowland loess deposits, North Iran

    Tamara Dulić, Jussi Meriluoto, Tamara Palanački Malešević, Violeta Gajić, Tamara Važić, Nada Tokodi, Igor Obreht, Bojan Kostić, Petar Kosijer, Farhad Khormali, Zorica Svirčev (2016)
    Biocrusts and adjacent sediments were collected from the so-called loess plateau of Northern Iran and the loess deposits on the foothills of Alborz Mountains. The mineralogical and granulometric analyses characterized sediments as quartz-rich clayey or sandy silts. Cyanobacterial diversity, colony morphology and grain stabilization were studied by light and scanning electron microscopy, which showed glue-like layers of cyanobacterial EPS and dense networks of filamentous cyanobacteria immobilizing finer and bigger grains, respectively. Amorphous, tuft and globular cyanobacterial colony structures were also detected. 15 cyanobacterial genera were ...
    Biokore, Cijanobakterije, Diverzitet, Cijanotoksini, Stabilizacija sedimenata, Les

  • The first record of nautiloids (Cenoceras intermedius) from the early Pliensbachian of Rgotina, (Getic nappe, eastern Serbia)

    Paul Țibuleac, Barbara V. Radulović, Marinko Toljić (2020)
    Cenoceras intermedius (J. Sowerby) is one of the most widespread species among the Early Jurassic nautiloid fauna and its geological range still controversial up to the present day. The specimen of Cenoceras intermedius from the sandy bioclastic limestones of Rgotina (Getic nappe of eastern Serbia), is a large half conch representing the phragmocone. Viewing our findings in light of previous results suggests the main morphological changes occurred during the ontogenetic evolution. The coiling starts with a round-square whorl section, ...
    Cephalopoda, Cenoceras intermedius, ontogenetic changes, geological range, northwestern Neo-Tethys, Pliensbachian