Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Nikolić Nikola D."'
Autor:
Živković-Marinkov Emilija M., Milisavljević Dušan R., Stanković Milan D., Filipović Gordana Lj., Bojanović Mila R., Nikolić Nikola D., Babac Snežana S.
Publikováno v:
Acta Stomatologica Naissi, Vol 37, Iss 84, Pp 2334-2334 (2021)
Introduction:In addition to the characteristic clinical picture of respiratory infection, patients with COVID-19 can also be diagnosed with oral manifestations. Aim: The aim of this study was to review current literature for the prevalence of changes
Externí odkaz:
https://doaj.org/article/0b970cb05b9540f2bf25195b26368cf0
Autor:
Miladinović Dragoljub L., Ilić Budimir S., Mihajilov-Krstev Tatjana M., Nikolić Nikola D., Milosavljević Violeta N.
Publikováno v:
Hemijska Industrija, Vol 66, Iss 4, Pp 541-545 (2012)
The antibacterial potential of essential oil from Serbian Sideritis montana L. (Lamiaceae) on different bacteria was investigated. The essential oil was obtained from air dried aerial parts of the plant with 0.03% (w/w) yield by hydrodistillation for
Externí odkaz:
https://doaj.org/article/92f100acd3124603a47d0f562492abc7
Autor:
Premović Pavle I., Todorović Bratislav Ž., Nikolić Nikola D., Pavlović Mirjana S., Đorđević Dragan M., Dulanović Dejan T.
Publikováno v:
Journal of the Serbian Chemical Society, Vol 71, Iss 6, Pp 639-659 (2006)
The Cretaceus-Tertiary (KT) boundary at Stevns Klint (the Højerup succession), Fiskeler, consists of a thin red clay layer overlain by a thick one of black marl. These two layers are made up mainly from cheto-smectite and biogenic calcite. The black
Externí odkaz:
https://doaj.org/article/8387290c9dfe43ac83fa4b670107bf21
Autor:
Premović Pavle I., Krsmanović Milena M., Todorović Bratislav Z., Pavlović Mirjana S., Nikolić Nikola D., Đorđević Dragan M.
Publikováno v:
Journal of the Serbian Chemical Society, Vol 71, Iss 7, Pp 793-806 (2006)
Geochemical analyses of trace metals (Ir, Ni and Zn) in the kerogen of the black marl of the Cretaceous-Tertiary boundary succession (Fish Clay) at Stevns Klint (Højerup Church) were undertaken. The data for this kerogen were in accordance with a pr
Externí odkaz:
https://doaj.org/article/9d7df7266d274eb7a00d12ff27384bf2
Publikováno v:
Journal of the Serbian Chemical Society, Vol 69, Iss 3, Pp 205-223 (2004)
The Cretaceous-Tertiary (KT) boundary transition at the Blake Nose Plateau recovered by ODP Leg 171B (site 1049, hole A, core 17X, section 2) contains an ejecta bed (thickness ca. 17 cm) marking a late Cretaceous asteroid impact. The nature and geoch
Externí odkaz:
https://doaj.org/article/549a08371c4b4a58b7d7094181680f2f
Autor:
Premović Pavle I., Nikolić Nikola D., Pavlović Mirjana S., Todorović Bratislav Ž., Đorđević Dragan M., Nikolić Ružica S., Lopez Liliana, Lomonaco Salvador
Publikováno v:
Journal of the Serbian Chemical Society, Vol 66, Iss 10, Pp 647-670 (2001)
Trace metals in the four discrete layers of the Cretaceous-Tertiary boundary (Fiskeler) at Stevns Klint (Denmark) are relatively well studied, yet much remains to be learned about them. Therefore, an integrated study of the trace (meteoritic Ir, p
Externí odkaz:
https://doaj.org/article/99e6e260263e4be7b86e089eab041d39
Autor:
Premović Pavle I., Nikolić Nikola D., Tonsa Ivana R., Dulanović Dejan T., Pavlović Mirjana S.
Publikováno v:
Journal of the Serbian Chemical Society, Vol 64, Iss 5-6, Pp 349-358 (1999)
High concentrations (up to 4000 ppm) of copper(II) porphyrins have been detected in the kerogen of the Cretaceous/Tertiary (KT) boundary informal type sediment, the Fish Clay, at Stevns Klint, Denmark. These pigments have also been found in the Da
Externí odkaz:
https://doaj.org/article/df518bed9a3b46d98943efb03d62cffc
Autor:
Marinkov, Emilija M. Živković, Milisavljević, Dušan R., Stanković, Milan D., Filipović, Gordana Lj., Bojanović, Mila R., Nikolić, Nikola D., Babac, Snežana S.
Publikováno v:
Acta Stomatologica Naissi; Dec2021, Vol. 37 Issue 84, p2334-2340, 7p
Autor:
Premović, Pavle I *, Nikolić, Nikola D, Tonsa, Ivana R, Pavlović, Mirjana S, Premović, Miroslav P, Dulanović, Dejan T
Publikováno v:
In Earth and Planetary Science Letters 2000 177(1):105-118
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