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-Reference-Cited by-同舟云学术

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

Published:2019-06 Issue: Volume:255 Page:163-187
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Andersson Stefan S.^ORCID,Wagner Thomas,Jonsson Erik,Fusswinkel Tobias^ORCID,Whitehouse Martin J.^ORCID

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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