Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Darivojka Ljubović Obradović"'
Autor:
Miodrag Banješević, Vladica Cvetković, Albrecht von Quadt, Darivojka Ljubović Obradović, Nebojša Vasić, Aleksandar Pačevski, Irena Peytcheva
Publikováno v:
Minerals, Vol 9, Iss 11, p 672 (2019)
This study aims at better constraining the link between magmatism and metallogeny in the south-easternmost sector of the Bor Metallogenetic Zone (BMZ), where the world-class copper and gold deposit of Čukaru Peki was recently discovered. The obtaine
Externí odkaz:
https://doaj.org/article/da27bb282a5c41eb944c3ef283a3c9cc
Autor:
Ivana Carević, Morteza Taherpour Khalil Abad, Ali Reza Ashouri, Monika Mirković, Petar Stejić, Darivojka Ljubović-Obradović, Ali Asghar Aryaei, Seyed Hamid Vaziri
Publikováno v:
Cretaceous Research
In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh Basin (northeast Iran), platform carbonates were deposited during the Barremian/Early Aptian in environments in the domain of the northern Alpine Teth
Publikováno v:
Geologica Carpathica
Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera The biostratigraphy of the Upper Cretaceous volcanoclastic-sedimentary formations cropping out
Publikováno v:
Glasnik Srpskog Geografskog Društva, Vol 90, Iss 1, Pp 1-16 (2010)
Glasnik Srpskog geografskog društva
Glasnik Srpskog geografskog društva
The Upper Barremian-Lower Aptian succession is recorded from a limestone sequence that crops out in the surrounding of Rakova Bara in the Carpatho-Balkanides range in northeastern Serbia. The micropalaeontological and sedimentological studies lead to
Publikováno v:
Studia Universitatis Babes-Bolyai: Geologia, Vol 48, Iss 2, Pp 133-139 (2003)
This note describes Coptocampylodon pantici, a new morpho species from Upper Cretaceous outcrops of the Pocuta region (NW Serbia). Based on the rudists in superincumbent calcarenites and planktonic foraminifers of the D. concavata Zone overlying the