Dating brittle tectonic movements with cleft monazite: Fluid-rock interaction and formation of REE minerals

Author:

Berger A.12,Gnos E.3,Janots E.4,Whitehouse M.5,Soom M.6,Frei R.2,Waight T. E.2

Affiliation:

1. Institute of Geological Sciences; University of Bern; Bern Switzerland

2. Department of Geosciences and Natural Resource Management (Geology Section); Copenhagen University; Copenhagen Denmark

3. Natural History Museum; Geneva Switzerland

4. ISTerre; Grenoble France

5. Laboratory for Isotope Geology; Swedish Museum of Natural History; Stockholm Sweden

6. Geotest; Zollikofen Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference43 articles.

1. L'extrème occidentale du massif de l'Aar;Baer;Bull. Soc. Neuchâtel Sci. Nat.,1959

2. A field-based estimate of the zircon fission-track closure temperature;Bernet;Chem. Geol.,2009

3. Bousquet , R. 2012 Metamorphic framework of the Alps

4. Geochronological evidence for continuous exhumation through the ductile-brittle transition along a crustal scale low-angle normal fault: Simplon Fault Zone, central Alps;Campani;Tectonics,2010

5. Nouvelles observations structurales au SW du massif de l'Aar entre Visp et Gampel;Dolivo;Beitr. Geolog. Karte Schweiz (N.F.),1982

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