Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Ladislav A. Palinkaš"'
Autor:
Todor Serafimovski, Goran Tasev, Sabina Strmić Palinkaš, Ladislav A. Palinkaš, Lazar Gjorgjiev
Publikováno v:
Geologia Croatica, Vol 69, Iss 1, Pp 101-119 (2016)
The paper presents data about geology, geochemistry, structure, genesis and specific features of the Bučim, porphyry Cu deposit with active mining in Macedonia. The porphyry mineralization (0.3 % Cu, 0.3-0.5 ppm Au) is spatially and temporarily asso
Externí odkaz:
https://doaj.org/article/0849856684bc4ee1ab0c1ca52da65f73
Autor:
Sabina Strmić Palinkaš, Ladislav A. Palinkaš, Magda Mandić, Zvjezdana Roller-Lutz, Zoltan Pécskay, Gani Maliqi, Vladimir Bermanec
Publikováno v:
Geologia Croatica, Vol 69, Iss 1, Pp 121-142 (2016)
The Trepča Pb-Zn-Ag skarn deposit in Kosovo is spatially and temporarily related to the phreatomagmatic breccia of Oligocene age (~23 Ma). The deposit shows features typical for skarn deposits worldwide, including a stage of isochemical metamorphism
Externí odkaz:
https://doaj.org/article/b29b073aaf644e399c4c8736d89df8e3
Autor:
Sabina Strmić Palinkaš, Ladislav A. Palinkaš, Maja Kuzmanović, Maša Martinić, Štefica Kampić, Dragana Dogančić, Jasmina Obhođaš
Publikováno v:
Geologia Croatica, Vol 66, Iss 2, Pp 129-142 (2013)
This paper presents the results of the sampling surveys carried out in order to evaluate the environmental impact of the Rude and the Sv. Jakob historical mining sites, NW Croatia. The studied polymetallic ore deposits are differing in the mineralogi
Externí odkaz:
https://doaj.org/article/07c9cfde52d64f96bb8dbe8e70e499d9
Autor:
Sabina Strmić Palinkaš, Vladimir Bermanec, Ladislav A. Palinkaš, Blažo Boev, Robert A. Gault, Walter Prochaska, Ronald J. Bakker
Publikováno v:
Geologia Croatica, Vol 65, Iss 3, Pp 423-434 (2012)
The epidote-bearing Čanište pegmatite and adjacent Upper Carboniferous granodiorites cut Precambrian gneises, at the western slopes of the Selečka Mts., the Eastern Pelagonian zone, FYRO Macedonia. The pegmatite exhibits zonal internal structure w
Externí odkaz:
https://doaj.org/article/9ae0e822985c4440ba42f84694af9db9
Publikováno v:
Geologia Croatica, Vol 46, Iss 1, Pp 145-155 (2010)
The evaluation of the heavy metal discharge from liming materials into the arable soil in NW Croatia is based upon the contents of Fe, Mn, Pb, Cu, Zn, Cd, Co and Hg in the studied carbonate raw materials, obtained under simulated conditions of the lo
Externí odkaz:
https://doaj.org/article/7a7fdebf8edc490a84566e4c971077fc
Publikováno v:
Geologia Croatica, Vol 46, Iss 1, Pp 97-106 (2010)
Syngenesis versus epigenesis in the Kupferschiefer genetic model is still a matter of controversy. The title of the article seems to be a paraphrase of a well-known paper by WEDEPOHL (1971), “Kupferschiefer as a prototype of syngenetic sedimentary
Externí odkaz:
https://doaj.org/article/0a1b10555c89459f969fd9da5841c3c8
Autor:
Ladislav A. Palinkaš, Ivan Jurković
Publikováno v:
Geologia Croatica, Vol 47, Iss 1, Pp 103-115 (2010)
Strata-bound barite deposits occur in Devonian dolomites, situated in the Mid-Bosnian Palaeozoic Schist Mountains. These contain barite as the main ore mineral (5.9 wt% SrSO4 on average and d34S= +8.3‰) which comprises 90-99 wt% of the bulk ores. T
Externí odkaz:
https://doaj.org/article/6bbac835770b48fda401ce46d80c7cd0
Autor:
Ladislav A. Palinkaš, Sibila Borojevic Sostaric, Sabina Strmić Palinkaš, Walter Prochaska, Jorge Spangenberg, Stella Cuna, Boris Šinkovec
Publikováno v:
Geologia Croatica, Vol 63, Iss 1, Pp 93-115 (2010)
Samoborska Gora Mts. is situated within the westernmost part of the Zagorje–Mid–Transdanubian zone of the Internal Dinarides. The Samoborska Gora Mts. predominantly consists of Permian unmetamorphosed siliciclastic sediments and evaporites, overl
Externí odkaz:
https://doaj.org/article/2d236d3db5b14874a19aaaeaa223fe49
Publikováno v:
Geologia Croatica, Vol 61, Iss 2-3, Pp 385-394 (2008)
The Darnó Unit within the Zagorje-Mid-Transdanubian Megaunit is an allochtonous part of Dinarides in NE-Hungary and represents a relict of the Neotethyan accretionary complex. It contains blocks of submarine basalts of Triassic age in turbiditic sed
Externí odkaz:
https://doaj.org/article/a4672b14f8e84cf0bdafd6d756b5ef42
Publikováno v:
Geologia Croatica, Vol 69, Iss 1, Pp 1-2 (2016)
Externí odkaz:
https://doaj.org/article/a0ede606ccf343f0bcc3b4b06e0c4c5a