Претрага

Упит dcterms_subject_txt:northwestern Neo-Tethys

138 items

  • Can the dynamics of a subducted slab account for the Upper Cretaceous magmatism in the Sava-Vardar Zone and Timok Magmatic Complex? A Numerical Modelling Approach

    Nikola Stanković, Ana Mladenović, Dejan Prelević, Vesna Cvetkov, Vladica Cvetković (2024)

  • Regional Strike-Slip Structures in the Internal Dinarides: Insights from the Zvornik Fault

    Ana Mladenović, Violeta Gajić, Kristijan Sokol, Dejan Prelević (2024)

  • Late Triassic radiolarians from the Grivska formation, internal Dinarides, SW Serbia

    Nikita Bragin, Liubov Bragina, Nevenka Đerić, Nataša Gerzina-Spajić (2019)
    Paleontology, Stratigraphy, Economic Geology, Geochemistry and Petrology, Geology, Geophysics, Geotechnical Engineering and Engineering Geology
    ... (ScHiD et al., 2008). Grey cherty limestone se- quences occur quite common in the Triassic and Jurassic sedimentary successions of the Western Tethys realm: similar depositional and diagenetic conditions led to the formation of grey cherty lime- stones elsewhere (SUDAR & GAwLICK, 2018). Geol ...
    ... booklet for sheet Prijepolje K 34-16 – in Serbian| Savezni geološki zavod, Beograd. DE WEVER, P. 1982. Radiolaires du Trias et du Lias de la Tethys (Systćmatique, Stratigraphie). Socićtć Gćolo- gique du Nord, 7: 1–599. DIMITRIJEVIĆ M.D., 1997. Geology of Yugoslavia. Geological Institute GEMINI ...
    ... (1), 17–27 Late Triassic radiolarians from the Grivska Formation, Internal Dinarides, SW Serbia Circum-Pannonian Region related to the initial Neo- tethyan rifting stage. In: VozAR, J., EBNER, E, VOZAROVA, A., HAASs, ]}., KovAcs, S., SUDAR, M., BIELIK, M. & PER6, Cs. (Eds.). Variscan and Alpine ...

  • Is the Sava-Vardar zone a remnant of an Upper Cretaceous ocen? Pro et contra

    Vladica Cvetković, Dejan Prelević, Ana Mladenović (2024)
    Neotethys, ocean closure, subduction
    ... consider the SVZ an Upper Cretaceous ophiolite [2], whereas others view it as a diffuse zone of intracontinental magmatism [3]. The three-year RECON TETHYS Project, supported by the Serbian Science Fund, aims at providing a detailed tectonomagmatic reconstruction of thc SVZ. As part of this project ...
    ... research is supported by funds provided by SRI based on Contract no. 451-03-66/2024- 03/200126, as well as Science Fund of Serbia, project, RECON TETHYS (7744807). VC appreciates the support of the Serbian Academy of Sciences and Arts (F9 and F17). REFERENCES 1. Pamić, J., (2002). The Sava-Vardar ...
    ... Boev, B., Božović, M., ... & Schmid, S. M. (2017). The Late Cretaceous Klepa basalts in Macedonia (FYROM)— Constraints on the final stage of Tethys closure in the Balkans. Terra Nova, 29(3), 145-153. 4. Cvetković, V., Šarić, K., Grubić, A., Cvijić, R., & Milošević, A. (2014). The Upper Cretaceous ...

  • Upper Cretaceous scaglia type limestone from Klepa Mts. (North Macedonia) - sedimentology and biostratigraphy

    Violeta Gajić, Milena Dunčić, Ana Mladenović, Dejan Prelević (2024)
    The research area is located in the central part of North Macedonia, in the area of the Klepa Mts. Based on sedimentological, micropaleontological and biostratigraphical investigations of samples from both the east and west side of the Klepa Mts., sedimentary rocks of the Upper Creaceous age are determined. During the latest Cretaceous, this area was dominated by the sedimentation of dominantly carbonate rocks with variable amounts of clastic components. From the tectonic point of view, investigated area belongs to the ...

  • 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 (2024)
    geohemija granata, retke zemlje, fluidne inkluzije, skarnovsko ležište Rudnik

  • 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
    ... and Africa-derived plates. The pre- sent-day SW-verging nappe stack (Fig. 1) records the opening and closure of cither one single branch of Neo- tethys (Bernoulli and Laubscher 1972; Schmid et al. 2008; Bortolotti et al. 2013) or alternatively, multiple oceanic branches (Dimitrijevic 1982; Karamata ...
    ... Geology, J3J, J, 233-236. Jolivet, L., Faccenna, C., Agard, P., Frizon de Lamotte, D., Menant, A., Sternai, P., and Guillocheau, F., 2015, Neo-Tethys geody- namics and mantle convection: from extension to compression in Africa and a conceptual model for obduction l: Canadian Journal of Earth ...
    ... Serbia. Global and Planetary Change, 103, 39-62. Tomljenović, B., Csontos, L., Mdrton, E., & Mirton, P. (2008). Tectonic evolution of the northwestern Internal Dinarides as constrained by structures and rotation of Medvednica Mountains. North Croatia: Geological Society, London, Special Publica- ...

  • U-Pb zircon geochronology of the Paleogene – Neogene volcanism in the NW Anatolia: Its implications for the Late Mesozoic-Cenozoic geodynamic evolution of the Aegean

    E. Yalçın Ersoy, Cüneyt Akal, Ş. Can Genç, Osman Candan, Martin R. Palmer, Dejan Prelević, İbrahim Uysal, Regina Mertz-Kraus (2017)
    The northern Aegean region was shaped by subduction, obduction, collision, and post-collisional extension processes. Two areas in this region, the Rhodope-Thrace-Biga Peninsula to the west and Armutlu-Almacık-Nallıhan (the Central Sakarya) to the east, are characterized by extensive Eocene to Miocene post-collisional magmatic associations. We suggest that comparison of the Cenozoic magmatic events of these two regions may provide insights into the Late Mesozoic to Cenozoic tectonic evolution of the Aegean. With this aim, we present an improved Cenozoic stratigraphy ...

  • Integrated Stratigraphy of the Middle–Upper Jurassic of the Krížna Nappe, Tatra Mountains

    Renata Jach, Nevenka Đerić, Špela Goričan, Daniela Reháková (2014)
    carbon and oxygen isotopes, radiolarians, calcareous dinoflagellates, radiolarites, Krížna Nappe, West ern Carpathians, Tethys
    ... Križna Nappe, 'Western Carpathians, Tethys. Manuscript received 11 November 2013, accepted 14 4pril 2014 INTRODUCTION Radiolarites are onc of the most typical facies of the Middle-Upper Jurassic successions in the Western Tethyan region. In the Alpine Tethys, the onset of biosiliceous sedi- ...
    ... to Early Cretaceous radiolarian biochronology of Tethys based on Unitary Associations. In: Baumgartner, P. O., O'Dogherty, L., Goričan, Š. Urquhart, E., Pillevuit, A. & De Wever, P. (eds), Middle Jurassic to Lower Cretaceous Radiolaria of Tethys: Occurrences, Systematics, Biochrono- logy. Memoires ...
    ... rassic radiolarites and associated deep-water carbonates were related to the breakup of Pangea and the opening ofthe Atlantic Ocean and the Alpine Tethys. Usually, the appear- ance of radiolarites was associated with sedimentation in basins with thinned continental crust, or in basins with oce- ...

  • Tеслапедиа као централна база библиографских података о Николи Тесли

    Ивана Ћирић, Сузана Топаловић, Биљана Лазић (2013)
    Циљ овог рада је да прикаже идеју и процес израде најкомплетније електронске библиографске базе о Николи Тесли, симболично назване Теслапедиа. Oвaквa бaзa би укључивaлa Teслину библиoгрaфиjу, кao и библиoгрaфиjу других o њeму. Сaм кoнцeпт рaзвoja Teслaпeдиe je видљив крoз двe глaвнe идeje. Првa идeja je зaснoвaнa нa пoстaвљaњу свих пoстojeћих библиoгрaфских јединица кoje Mузej пoсeдуje нa oдрeђeну вeб-лoкaциjу a другa, пoдjeднaкo вaжнa, oглeдa сe у мoгућнoстимa дaљeг рaзвoja и нaдгрaдњe сaмe структурe базе придруживaњeм нoвих библиoгрaфских пoдaтaкa. Oвa бaзa ...
    библиографије
    ... прес-клипинг Николе Tесле, 3. Tesla Collection, 4. Нео бја вље на би бли о гра фи ја Ми ло ва на Ма ти ћа, 5. Те сли на лич на би бли о те ка. Ме ђу њи ма раз ли ку је мо сле де ће: a) Из во ре ко ји су у осно ви на ста ли као би бли- о гра фи је (Нео бја вље на би бли о гра фи ја Ми- ло ва на Ма ти ...
    ... сва- кој де фи ни ци ји оста ју бли ско по ве за ни5. Ин фор- ма тич ка ера, раз вој но вих тех но ло ги ја и ди ги тал- них ме ди ја отво ри ли су нео гра ни че не мо гућ но сти у обла сти до ку мен то ва ња и пре зен та ци је знaњa као пр вом ко ра ку у про це су ње го вог очу ва ња и дисeминaциje ...
    ... до у ми це се умно жа ва ју у слу ча ју ра зно- род них збир ки ко је су део јед не це ли не, ту су не- при ме њи ва по је ди нач на ре ше ња јер је нео п ход но одр жа ти по ве за ност свих ко лек ци ја и му зе а ли ја. При мер ком плек сне уста но ве за шти те кул тур них до ба ра ко ја у свом фон ...

  • Strain partitioning around an indenter during oroclinal bending: kinematics of the Circum-Moesian fault system of the Carpatho-Balkanides

    Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga (2021)
    ... orocline situated in the south and west. The southern orocline of the Carpatho-Balkanides orogenformed during the Cretaceous closure of the Alpine Tethys Ocean and collision of the Dacia mega-unit with the Moesian Platform. Following the main orogen-building processes, the Carpathianssubduction and Miocene ...

  • Варијанта решења примене екрана у заштити Површинског копа Дрмно од вода

    Дарко Станић (2024)
    Због напредовања рударских радова, Површински коп Дрмно се приближава кориту реке Дунав на северној страни. Постоје две могуће границе површинског копа, а због сигурне експлоатације потребно је одабрати квалитетно предодводњавање.То је могуће израдом водонепропусног екрана.Одрађени су прорачуни прилива подземних вода у коп за обе локације површинског копа, применом водонепропусног екрана. Локација 1 има контуру површинског копа по постојећој Студији изводљивости, а Локација 2 има контуру копа на основу резултата нових геолошких истраживања. Свака локација има по две варијанте предодводњавања ...
    одводњавање, водонепропусни екран, површински коп Дрмно
    ... OH mmpuny o,r 1,0 m, a ocTaji neo eKpaHa y JUykHHu o,JI 1.998,6 m BMao Ou mmipuHy eKpaHa oJ 0,8 m. OO3HpoM Ha nyOHHy H mupuHy eKpaHa panune O 3 amme. JenHa MammHa Og HapaljuBana Jeo ekpaHa nyOHHe no 40 m, unja OB mpupuna Ouna 0,8 m, npyra amuHa O apaljaBana neo eKkpaHa o NyOMHe 80 m, ugja OH mupuHa ...
    ... Ou mmipHHy on 1,0 m, a ocrajn neo eKpaHa y JUy?)xHHH OJ 3.559 m uMao O mmapuHy ekpaHa oJ 0,8 m. O03HpoM Ha JnyOHHy H mupuHy cKpaHa pame OH 2 MammHe. JenmHa MammHa OH MHy3pabuBama eo eKpaHa NyOuMHe mo 40 m, uuja O mpupuHa Ouzma 0,8 m, a npyra MamaHa Og H3pabuBaa neo ekpaHa o nyOaHe 80 m, unaja ...
    ... oDame. IipnHa craHMma Komamre wyarpabeHa je Ha HMH3BOJMHOJ Iperpaju perynacaHor Mmema J[yHaBma H OM CC BOJa HpeHyMIaBa HeHOcCpeJiHO H3a Hperpajie y neo ZJlyHaBia KOjH Je y KOHTAKTy Ca BOJIOTOKOM /lyHaBa. HoBa ıipnHa craHHma Konuimrre Je y pany o 1980. ronuHe H M50M Ce BOJIOCTAJ y peryJ11CaHOM KopuTy ...

  • Callovian (Middle Jurassic) Sphriganaria (Brachiopoda) from the Jordan Valley (Middle East)

    Howard R. Feldman, Barbara V. Radulović, Fayez Ahmad (2023)
    Brachiopods, Middle Jurassic, Sphriganaria, shell microstructure, Ethiopian Province

  • Pannonian Basin, Pannonian Basin System and Pannonian realm - three different concepts

    Dejan Radivojević (2019)
    Centralni Paratetis, neogen, Panonski basen, Sistem panonskog basena, Panonska oblast
    ... The Central Paratethys occupied this space starting from the Lower Miocene until the definitive connection break with the southern remnant of Tethys - the Mediterranean Sea, that occurred during the Upper Miocene (Panonnian) time. During this period, our part of the Pannonian Basin passed from ...

  • Definisanje strukturnih odnosa primenom postupka horizontalni gradijent

    Snežana Ignjatović, Ivana Vasiljević, Natalija Jovanović (2019)
    Različiti postupci matematičkih transformacija se mogu primeniti na gravimetrijskim i magne tometrijskim podacima, kako bi se na istražnom terenu definisali strukturno-tektonski odnosi. U radu su prikazani rezultati dobijeni korišćenjem postupka horizontalni gradijent i ukupni horizontalni gradijent na gravimetrisjkim podacima. Navedeni postupci su pomogli da se detektuju kontakti sa velikim padnim uglom (vertikalni ili subvertikalni kontakti), koji se mogu interpretirati kao rasedi. Za test područije uzet je istražni prostor koji se nalazi na jugoistoku Srbije u okolini Vranjskog basena. Položaji ...
    gravimetrijski podaci, matematičke transformacije, rased, Vranjski basen
    ... gradijent i postupk ukupni horizontalni gradijent. Vranjski basen se nalazi u jugoistočnom delu Sr- bije, a formiran je kao depresiona struktura tokom neo- gena i kvartara. Vranjski rov je složen depresioni pro- stor sa dominatnim centralnim delom, koji se sastoji od jedne relativno uzane zone spuštene ...
    ... Interpretation of Gravity and Magnetic Data, Getech Kitson House Elmete Hall Leeds, UK, 2007. [8] Marović M, Toljić M, Rundić Lj, Milivojević J, Neo- alpine Tectonics of Serbia, Serbian Geological So- ciety, Beograd, 2001. SUMMARY THE APPLICATION OF HORIZONTAL GRADIENT FOR DEFINING STRUCTURAL ...

  • Evidence of Variscan and Alpine tectonics in the structural and thermochronological record of the central Serbo-Macedonian Massif (south-eastern Serbia)

    Milorad D. Antić, Alexandre Kounov, Branislav Trivić, Richard Spikings, Andreas Wetzel (2016)
    General Earth and Planetary Sciences
    ... opening of the Meso- zoic Tethys. The greenschist facies retrogression in the Lower Complex probably occurred in the Early Jurassic (195 + 1 Ma), and it was related to the thermal processes in the overriding plate above the subducting slab of the Mesozoic Tethys Ocean. Keywords Serbo-Macedonian ...
    ... 2002; Karamata 2006; Stampfli et al. 2013). A similar evolution took place again during the Alpine orog- eny with polyphase opening of the Mesozoic Tethys and its consequent closure involving collision of multiple crustal segments (e.g. Robertson et al. 1991; Ricou 1994; Schmid et al. 2008; Stampfli ...
    ... margin (ca. 250 Ma; De Wet et al. 1989; Himmerkus et al. 2009b; Peytcheva et al. 2009b) that eventually led to the opening of the Mes- ozoic Tethys west of the SMM (Robertson et al. 1991; Kar- amata and Krstić 1996; Pe-Piper 1998; Stampfili et al. 2002; Burg 2012). In western part of the central ...

  • Основе конструисања

    Бобан Анђелковић, Милош Танасијевић, Филип Милетић (2023)
    Машинске конструкције

  • English for Geology Students. 2

    Lidija Beko (2023)
    Engleski jezik
    ... caa Table of contents • Unit5 • SURFACE WATERS AND GLACIERS Partl SUREFACE WATER....... ttt ttt 122 Vocabulary....n.MOORe. ... o - W ... .. NEO 125 Reading Comprehension.......... iii 126 Part,2 RBGLAGIERSL. .. a e ddv do M, a . . -M JM 128 'Vocabulary...e.....RM I o N i. y- k 131 Reading ...

  • English for Geology Students. 1

    Lidija Beko (2023)
    Engleski jezik
    ... Table of contents • Unit5 • ROCK CYCLE, IGNEOUS ROCKS AND VOLCANOES Partl ROCKCYCLE........ ttt tttv 126 Vocabulary....n.MOORe. ... o - W ... .. NEO 128 Reading Comprehension.......... iii 129 Part 2 |ŽČIGNEOUS ROCKS.... . a v MM . .O . M, 130 'Vocabulary....e.. ...R ... a o . N i a y- k 133 ...

  • Trans-Lithospheric Diapirism as a Possible Mechanism for Ophiolite Emplacement?

    Nikola Stanković, Taras Gerya, Vladica Cvetković, Vesna Cvetkov (2024)