Apatite as a tracer of the source, chemistry and evolution of ore-forming fluids: The case of the Olserum-Djupedal REE-phosphate mineralisation, SE Sweden
Author:
Funder
GeoDoc Graduate Programme
Academy of Finland
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference147 articles.
1. Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon;Andersen;J. Geol. Soc. Lond.,2009
2. Mineralogy, paragenesis and mineral chemistry of REE’s in the Olserum-Djupedal REE-phosphate mineralization, SE Sweden;Andersson;Am. Mineral.,2018
3. Origin of the high-temperature Olserum-Djupedal REE-phosphate mineralisation, SE Sweden: a unique contact metamorphic-hydrothermal system;Andersson;Ore Geol. Rev.,2018
4. Formation of hydrothermal REE-phosphate deposits;Andersson,2019
5. The chloride source for atacamite mineralization at the Radomiro Tomic porphyry copper deposit, northern Chile;Arcuri;Econ. Geol.,2003
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