engleski

Repetitio est mater studiorum: Do the orogeneses repeat their P-T patterns through the metamorphism in the Slavonian Mts. (Tisia Mega-Unit)?

During geological history large scale geotectonic movements produced vaguely similar clockwise P-T paths reaching different maximal P-T values. Obtained P-T paths and geothermobarometric data in the Slavonian Mts. support nappe stacking model for Alpine orogenesis, convergence-related environment and tectonic exhumation with later intrusion of granites during Variscan events and docking (rather than classic subduction due to a deducible geothermal gradient ~15 °C/km) of a continental plate (Gondwana) and another underthrusted smaller (micro)plate in the Early Paleozoic.

Early Paleozoic; Variscan; Alpine; Gondwana; Alpine belt; P-T path; Slavonian Mts.

Dio prikazanih istraživanja napravljen je u sklopu projekta HRZZ IP-2014-09-9541