| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8908605 | Tectonophysics | 2018 | 61 Pages |
Abstract
Haematite, the main carrier of the palaeomagnetic signal in the studied area, was shown to recrystallize at temperatures above 120â¯Â°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.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Jan ÅrodoÅ, Aneta A. Anczkiewicz, István Dunkl, Igor VlahoviÄ, Ivo VeliÄ, Bruno TomljenoviÄ, Tadeusz Kawiak, MichaÅ BanaÅ, Hilmar von Eynatten,