SVIBOR - Papers quoted in CC - project code: 1-09-289

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Papers quoted in Current Contents on project 1-09-289

Quoted papers: 9
Other papers: 21
Total: 30

Title: Eoalpine to Neoalpine magmatic and metamorphic processes in the northwestern Vardar Zone, the easternmost Periadriatic Zone and the southwestern Pannonian Basin.

Authors:: Pamić, Jakob (98874)

Journal: Tectonophysics
ISSN: 0409-51
Volume: 226
Year: 1993
Pages: from 503 to 518
Language: engleski
Summary: The occurrence of Eoalpine-Neoalpine, genetically differentgranitoids and penecontemporaneous volcanics are characteristicfor the Vardar Zone. Spatially associated UpperCretaceous-Paleogene sediments were progressively metamorphosedunder medium-pressure conditions. The high-pressure metamorphismwas related to an Eoalpine event. Eoalpine and Mesoalpinemagmatism and metamorphism may have taken place along asubduction zone. The easternmost parts of the Periadriatic Zoneare characterized only by Oligocene granitoids and andesitesgenetically related to estension. The southwestern PannonianBasin contain products of four pulses of Mesoalpine and Neoalpinesynsedimentary volcanic activity represented by predominantbasalt-andesites, trachyandesites and dacites. Thispost-subduction volcanism was closely connected with the cyclicmarine ingressions in the Pannonian Basin.
Keywords: Vardar Zone, Periadriatic Zone, south Pannonian Basin, magmatism, metamorphism, Eo-, Mezo- and Neoalpine, subduction, extension

Title: Alpinski A-graniti kolizijskog područja najsjevernijih Dinarida i Panonskog bazena, Jugoslavija

Authors:: Pamić, Jakob (98874); Lanphere, Marvin

Journal: Neues Jahrbuch fuer Mineralogie, Abhandlungen
Number: 2
ISSN: 0077-7757
Volume: 162
Year: 1991
Pages: from 215 to 236
Number of references: 19
Language: engleski
Summary: Alpine A-type granites cut Upper Cretaceous basalts and rhyolites or co-evel low-grade metamorphic rocks. On the granites and rhyolites a Sr-isochron age of 71,2 Ma was obtained. Granites are represented by alkali-feldspar varieties which, according to major- and trace-element contents belong to the A-type granite family. REE concentrations are slightly lower than in A-type granites elsewhere. Sr-isotopic composition suggests that the granites were generated in partly-melted continental crust.
Keywords: Požeška gora Mt., Prosara Mt., bimodal basalt-rhyolite formation, alpine low-grade metamorphic rocks, Sr-izochron, microprobe chemical composition, rock classification, geochemistry, REE, petrogenesis

Title: Gornjokredne bimodalna vulkanska asocijacija iz južnih dijelova Panonskog bazena u Slavoniji (sjeverna Hrvatska)

Authors:: Pamić, Jakob (98874); Bullen, Thomas; Lanphere, Marvin; McKee, Edwin

Journal: Neues Jahrbuch fuer Mineralogie, Abhandlungen
ISSN: 0077-7757
Year: 1996
Pages: from 1 to 20
Number of references: 38
Language: engleski
Summary: The paper presents informations for bimodal basalt-rhyolite suite and associated A-type granites whose late Cretaceous geological age is supported by Rb-Sr and K-Ar data. The petrology and geochemistry for basalts and rhyolites are defined in detail using microprobe analyses, major and trace element analyses and stable isotope composition. Field relationship and all analytical data indicate that the Upper Cretaceous volcanism which was genetically related to final stages of subduction produced A-type rhyolites of crustal origin and basalts of upper mantle origin.
Keywords: bimodal basalt-rhyolite suite, Southern Pannonian Basin, geological and isotopic ages, microprobe analyses, major and trace elements, stable isotopes, relict magmatic arc, subduction processes

Title: Tercijarne vulkanske stijene iz južnih dijelova Panonskog bazena u Hrvatskoj

Authors:: Pamić, Jakob (98874); McKee, Edwin; Bullen, Thomas; Lanphere, Marvin

Journal: Geological Society of America Bulletin
ISSN: 0016-7606
Year: 1995
Pages: from 1 to 30
Number of references: 43
Language: engleski
Summary: Tertiary volcanic rocks are related to sequentional tectonic processes which took place along the northern margin of the Dinarides after their Eocene uplift when subduction processes ceased. The oldest are Egerian-Eggenburgian andesites related to transpression which were followed by Karpathian trachyandesites related to initial rifting and extensional evolution of the Pannonian Basin. The strongest was Badenian volcanism which gave mostly basalts and andesites which were followed by postbadenian alkalic basalts. These four Tertiary volcanic groups were studied in detail using different analytical procedures (K-Ar and stable isotope measurements, microprobe analyses, major- and trace elements) and all analytical data obtained indicate their complex petrological evolution related to active continental margin.
Keywords: Oligocene and Miocene volcanism, South Pannonian Basin, geological and isotopic ages, microprobe analyses, major- and trace-elements, stable isotope composition, subduction, rifting, extension


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