Naslov
Vrlo niski do niski stupanj metamorfizma Radlovačkog kompleksa, Papuk
(Very low- to low-grade metamorphism of Radlovac Complex, Mt. Papuk)

Autori
Balen, Dražen ; Sabljak, Nenad ; Tibljaš, Darko

Vrsta, podvrsta i kategorija rada
Poglavlja u knjigama, znanstveni

Knjiga
5. Hrvatski geološki kongres, Vodič ekskurzija

Urednik/ci
Horvat, Marija ; Galović, Lidija

Izdavač
Hrvatski geološki institut

Grad
Zagreb

Godina
2015

Raspon stranica
68-70

ISBN
978-953-6907-50-1

Ključne riječi
slejt, filit, metadijabaz, metabazalt, Tisica, Radlovački kompleks, Papuk, Slavonske planine
(slate, phyllite, metadiabase, metabasalt, Tisica, Radlovac complex, Papuk Mt., Slavonian Mts.)

Sažetak
The outcrops of the Radlovac metamorphic complex (also known as the Radlovac formation) can be found in a broad region of the Papuk and Psunj Mts. On the way of our excursion first outcrops are in the Tisica quarry and along the road Velika - Slatinski Drenovac just a km north from Velika. Type locality is on the northern side of Mt. Papuk along the Radlovačka Rijeka valley, with interesting localities at Hercegovac and Žervanjska. Very low grade (VLG) metamorphic rocks are mostly slates and schistose metasandstones with subordinate phyllites, quartzites and schistose metaconglomerates. The complex is intruded by smaller bodies of metadiabase and ophitic metagabbro. Metamorphism reaches temperature range from the upper anchizone (approx. 250 °C) to the low temperature part of epizone (300 °C) and pressures 2-3 kbars.

Izvorni jezik
Hrvatski

Znanstvena područja
Geologija

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