Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi

Hercynian I-type and S-type granitoids from the Slavonian mountains (southern Pannonian Basin, northern Croatia) (CROSBI ID 80012)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Pamić, Jakob ; Lanphere, Marvin ; Belak, Mirko Hercynian I-type and S-type granitoids from the Slavonian mountains (southern Pannonian Basin, northern Croatia) // Neues Jahrbuch für Mineralogie. Abhandlungen, 171 (1996), 2; 155-176-x

Podaci o odgovornosti

Pamić, Jakob ; Lanphere, Marvin ; Belak, Mirko

engleski

Hercynian I-type and S-type granitoids from the Slavonian mountains (southern Pannonian Basin, northern Croatia)

Two genetically different groups of Hercynian granitoids occur in the Slavonian Mountains which are included in the southern Pannonian Basin. I-type granitoids occur in Barrovian-type progressive metamorphic sequences which originated during the Hercynian orogeny from the Late Silurian to Lower Carboniferous magmatic-sedimentary complex. S-type granitoids, enriched in incompatible trace elements, are accompanied by penecontemporaneous migmatites which originated from rocks of the same progressive metamorphic sequences and lower continental crust. I-type granitoids are represented mostly by granodiorite and monzogranite impoverished in incompatible trace elements, with rare diorite and monzodiorite and basic to intermediate rocks. Hercynian age of the crystalline rocks is supported by numerous K-Ar, 40Ar-39Ar and Rb-Sr measurements carried out mostly on monomineralic concentrates. About 20 representative samples of S-type and I-type granites and associated rocks were selected from over 1000 samples and analyzed in detail. Although most major and trace element diagrams do not provide the best genetic discrimination between the Slavonian granitoids, Sr and O isotope composition, REE data and some other data for the S-type granitoids are indicative of their sedimentary and continental crust source, whereas the I-type granitoids were derived by partial melting of the upper mantle with slight crustal contamination.

radiometric ages; Barrovian sequences; I-type and S-type granites; major and trace elements; REE; radiogenic and stable isotopes; petrogenesis

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

171 (2)

1996.

155-176-x

objavljeno

0077-7757

2363-7161

Povezanost rada

Geologija

Indeksiranost