Претрага

Упит dcterms_subject_txt:L’dži locality

65 items

  • A contribution to the understanding of hydrochemical properties of thermomineral water on the L’dži locality (eastern part of North Macedonia)

    Hristina Petrova, Katarzyna Wątor, Piotr Rusiniak, Boris Vakanjac, Vesna Ristić Vakanjac, Ewa Kmiecik (2023)
    Regarding the aspect of mineral, thermo-mineral, and thermal waters, on the territory of the Republic of North Macedonia, there are 65 registered locations, of which 8 are categorized as spas. This includes the Kežovica spa, also known as the Štipska spa. In the vicinity of Kežovica Spa is the thermo-mineral L’Dži spring with mineralization around 1.3 g/L and the water temperature at the time of sampling was 50.1 °C. Spring L’Dži is generated by a fault structure and is ...
    thermo-mineral water, water chemistry, hydrochemical properties, L’dži locality, North Macedonia.

  • Mining activites through history at Avala locality

    Crnogorac Luka (2016)

  • The Mine Non Sulfid Ore From Prlovi-2 Locality Characterization

    Lazić Predrag, Tomanec Rudolf, Miković B. (2011)

  • New data on radiolarian assemblages from the Krš Gradac locality (SW Serbia)

    Đerić Nevenka, Chiari Marco, Gerzina Nataša (2012)

  • The mine ore from Prlovi-2 locality preliminary flotation tests

    Lazić Predrag, Tomanec Rudolf, Kostović Milena, Miković Branislav (2011)

  • Polymetallic Cu-Bi-(Pb-Zn-Co-Ag) mineralization of the Perin Potok locality near Bor, Serbia

    Pačevski Aleksandar, Šarić Kristina, Cvetković Vladica (2013)

  • Pinite-cordierite from spotted slate of the Brajkovac contact metamorphic aureole (Dudovica Locality, Central Serbia)

    Vasković Nada, Nikić Zoran, Srećković Batoćanin Danica, Erić Suzana, Memović Emin (2013)

  • Depth estimation of archeological objects using Euler 3D deconvolution of magnetic data

    Vesna Cvetkov, Ilija Vasiljević, Mirko Petković (2015)

  • Реликти океанске коре на Фрушкој гори, габрови и базалти Јаска -Relics of the Ocean Crust at the Fruska Gora Mountain, Gabbros and Basalts in the Jazak locality

    Срећковић Батоћанин Даница, Васковић Нада, Матовић Весна, Ерић Сузана (2010)

  • Палеомагнетски резултати из Тимочког магматског комплекса, Источна Србија

    Весна Лесић, Емо Мартон, Драган Лукић, Весна Цветков (2018)
    ... able  to calculate  statistically well defined locality mean directions for 7 locality/sites out of 13. The samples from six loca‐ lites  /sites were unstable during demagnetization and  for  that  reason  it was not possible  to define a  site/locality mean direction for them. The overall‐mean pale ...
    ... o demagnetize the rest of the samples from each locality/site.  The demagnetization curves were analyzed for  linear segments  (Kirschvink 1980) and the segments or  selected steps of demagnetization were subjected to statistical evaluation on locality level (Fisher 1953).  Overall‐mean paleomagneti ...
    ... c direction was calculated from the in situ locality mean directions as well as  from those after tilt corrections  in order to find out  if the magnetization  is of pre or post–folding age.  Magnetic mineralogy experiments included Curie‐point measurements, the stepwise isothermal magne‐ tization  (IRM)  ...

  • Post Early Miocenevertical-axis clockwise rotation in the West Vardar Zone of Serbia

    Vesna Lesić, Emo Marton, Vesna Cvetkov, Dragana Jovanović (2018)
    ... specimens from each locality/site. Magnetic mineralogy experiments were carried out on selected specimens. The demagnetization curves were then analyzed for linear segments which were used for statistical evaluation on locality/site level. The fold/tilt test was carried out on locality (when applicable) ...
    ... In this 160 km long strip we sampled on the north in the wider Rudnik Mts. area seven localities of Late Cretaceous micritic limestones and one locality of flysch and seventeen sites of Oligocene-Earliest Miocene igneous rocks of different composition. In the south, ın the wider Kopaonik Mts. Area ...
    ... and regionallevel. The obtained results show that the remanent magnetization both in the igneous rocks and sediments resides in magnetite. The locality mean directions for Late Cretaceous sediments are well defined and the remanenceis of post tilting: age. For both the Oligocene-Earliest Miocene ...

  • Micro- to nanoscale textures of gold in arsenopyrite and scorodite from the As-Au-Bi assemblage of Drenjak locality (Serbia)

    Ivana Jelić, Janez Zavašnik, Marina Lazarov, Alena Zdravković, Sabina Kovač, Jovica Stojanović, Aleksandar Pačevski (2023)
    Arsenopyrite and pyrite are important carriers of Au that is present in the form of microscopic and “invisible” gold. Such gold can be expected to be released upon the process of oxidation of these sulfides. In studied gold mineralization at Drenjak, related to the granitoids of the Oligocene-Miocene Kopaonik Ore District, the main arsenopyrite-pyrite-(bismuthinite) sulfide assemblage was formed in the quartz bodies and partly replaced by scorodite (FeAsO4·2H2O) and Bi-arsenate. With only up to 5 ppm of gold recorded ...
    Economic Geology, Geochemistry and Petrology, Geology

  • Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications

    Vesna Lesić, Emo Márton, Violeta Gajić, Dragana Jovanović, Vesna Cvetkov (2018)
    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 ...
    Paleomagnetism, Clockwise rotation, Dinarides, West Vardar zone
    ... sensu Karamata (2006), or in other words to the West Vardar and Jadar–Kopaonik units sensu Schmid et al. (2008). Only a single locality (Cretaceous limestone at locality No. 8, see Fig. 2) is located in the East Vardar unit. The early geological and tectonic history of the Vardar zone is not of direct ...
    ... corrections (bold in Table 1). Five of them exhibit a tight cluster; locality 6 seems to be an outlier. While we have no direct evidence for the presence of hematite (carrying present overprint) in the white specimens from locality 6 (Fig. 4, specimen 4414B and Fig. 5, specimen 3968B), even a tiny ...
    ... 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 V. Lesić et al. Table 1 Wider Rudnik Mts. area, Cretaceous sediments Locality Lat. N Lithology n/no D° r° k dtgs° Ss «DS 1 Kk lgs° dip Age Lon. E 1 Struganik upper quarry 44°11'13” Limestones white, greyish 9/22 211.8 — 491 ...

  • A contribution to the knowledge of facial diversity of Badenian sediments in the Belgrade area

    Filip Anđelković, Dejan Radivojević (2018)
    baden, Beograd, facije, facijalna raznovrsnost, sedimenti
    ... ransgression.    CONCLUSION    Because of  its facial diversity, the Belgrade area can be considered as a second type  locality of  the Badenian stage. The original type locality is the Vienna basin (Anđelković M., 1987).   In the place of strictly delimited facies and subfacies, some transitional ...
    ...  further subdived  into three subfacies:  Lithothamnium‐bryozoan  limestone,  Amphistegina  limestone  and  Cerithium  limestone.  On  the  type  locality of these  limestones, the Leitha mountain (located  in the vicinity of Vienna), similar facies have  been found (Wiedl et al., 2012; Rundić et al ...
    ... istegina facies (Wiedl et al., 2012).  Lithothamnium‐bryozoan  limestones  form  two  big  and  one  smaller  bioherm  (picture  1).  The  type  locality  of  the  Tašmajdan  limestones  is  Tašmajdan, which once was  a quarry  from which  these  limestones have been exploited as a ‐‐‐‐.  Amphistegina  ...

  • Palaeoflora of Kamenica (Pranjani Basin, western Serbia)

    Zorica Lazarević, Ljubica Milovanović, Jelena Milivojević, Ivana Vasiljević (2019)
    Palaeofloras of the Paleogene in Serbia are relatively rare, especially in comparison with floras from Neogene sediments. Most Paleogene phytoas sociations from the territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleo gene phytoassociations.The palaeoflora from Kamenica is characterized with leaf imprints larger than in other ...
    макрофлора, млађи олигоцен, Прањански басен, Каменица
    ... territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleo- gene phytoassociations ...
    ... MiLiVojEVić & iVAnA VASiLjEVić Geol. an. Balk. poluos., 2019, 80 (2), 53–6354 Fig. 1. Position of Čačak-Kraljevo Basin and position of palae- oflora locality. Fig. 2. Gravity anomaly map (Dg) with the position of Neogene basins (yellow shaded areas) and the location of the paleontolog- ical site Kamenica ...
    ... charac- terized with considerable depth. Palaeoecology and palaeoclimatology about one hundred leaf imprints have been col- lected at the Kamenica locality. considering the rel- atively small number of specimens, there is a rich taxonomical diversity (Table 1). analyzing the character of the leaf imprints ...

  • Paleomagnetic study of Jurassic-Early Cretaceus sediments in the Danibicum of Eastern Serbia

    Vesna Cvetkov, Emo Marton, Vesna Lesić, Dragana Tomić (2015)
    ... were analyzed for linear segments which were used for statistical evaluation on locality level. In order to determine if the obtained remanent magnetization for the localities is of pre or post–folding age on locality level and regional level we performed the fold tests. As a results of de ...
    ... demagnetization, well defined, apparently single component remanences were isolated. The statistical parameters on locality level are usually excellent. Both the present and the earlier studies in Romania for the Jurassic defined remanences of post- deformational age. The overall mean direction for ...

  • 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
    ... slope or on a proximal oceanic bottom. They are comparable with the Potschen Formation ({type locality) in the Northern Calcareous Alps or with grey cherty limestone of Meliata unit (type locality) in the Western Carpathi- ans [GAWLICK et al., 2016). The age of Lim river succession is dated ...
    ... and radiolarians, and did not yield any macrofossils. Micropa- laeontological research of Upper Triassic siliceous rocks was performed at the locality Lim River, in the vicinity of Bistrica Village in SW Serbia. Radiolarian assemblages are characterized by such species as Capnodoce anapetes DE ...
    ... melange ——— Late Jurassic obduction Sediments of the passive margin of Adria (Jurassic) Sediments of the passive margin of Adria (Pz and T) Locality Lim The Grivska Formation was informally introduced by DIMITRIJEVIĆ: & · DIMITRIJEVIĆ (1987, 1991): the definition of this formation was ...

  • Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone

    Emő Márton, Marinko Toljić, Vesna Cvetkov (2022)
    The Vardar Zone is a product of the Triassic-Jurassic opening of the Neotethys, Jurassic obduction, Late Cretaceous/Paleogene consumption of the oceanic crust and continental collision. During the last process, the Eastern Vardar Zone was thrust over the Central and eventually both onto the Western Vardar Zone. The present paleomagnetic and structural study provided new results from the first two zones in the Belgrade area. The younger set of data, together with published ones from the third zone, provide firm ...
    Adria–Europe suture, Vardar Zone, Paleomagnetism, Thrusting, Vertical axis rotation

  • Clockwise rotation in the Serbian segment of the Vardar zone and in the Danubicum of Eastern Serbia - tetonic implication

    Vesna Lesić, Emo Marton, Vesna Cvetkov, Dragana Tomić (2015)

  • Composition of organic matter and thermal maturity of Mesozoic and Cenozoic sedimentary rocks in East Herzegovina (External Dinarides, Bosnia and Herzegovina)

    Nikoleta Aleksić, Aleksandar Kostić, Miloš Radonjić (2021)
    This paper presents the first data on the organic matter and thermal maturity of Mesozoic and Cenozoic sedimentary rocks in the East Herzegovina region of the External Dinarides. Representative, organic-rich samples from outcropping sedimentary rocks of different ages in the area (Triassic to Neogene) were selected and analysed. The organic matter was studied by Rock-Eval pyrolysis and under the microscope in reflected non-polarized light and incident blue light. The results obtained show the presence of different types of organic ...
    nafta i gas, Rock-Eval, refleksija vitrinita, maceral, termička zrelost
    ... vitrinite re�ectance were performed on the sample from Avtovac. �e sample from the Necvijeće locality had no re- liable phytoclasts for the measurement of re�ectance. �e results show that the Avtovac locality had a lower mean re�ectance of 0.41% Rr (huminite), corresponding to the immature stage. It ...
    ... vitrinite reflectance were performed on the sample from Avtovac. The sample from the Necvijece locality had no re- liable phytoclasts for the measurement of reflectance. The results show that the Avtovac locality had a lower mean reflectance of 0.41% Rr (huminite), corresponding to the immature stage. It ...
    ... (Carnian) were collected from two adjacent localities in the Lastva Anticline: Klobuk, and Župa (Fig. 1; Table 1). Samples were Sample No. Age Locality TOC S1 S2 S3 HI T max 1 T Klobuk 3.74 0.06 14.00 2.34 374 437 2 T Klobuk 2.81 0.05 9.35 3.17 333 439 3 T Župa 0.83 0.08 4.19 0.36 505 424 4 T ...