Thermal history of the central part of the Karst Dinarides, Croatia: Combined application of clay mineralogy and low-T thermochronology

Haematite, the main carrier of the palaeomagnetic signal in the studied area, was shown to recrystallize at temperatures above 120 °C, which explains the appearance of secondary magnetization well below the Curie point of haematite, such as reported recently in the Central Velebit Mt. area.