The origin and evolution of V-rich, magnetite dominated Fe-Ti oxide mineralization; Northwest River Anorthosite, south-central Labrador, Canada-Reference-Cited by-同舟云学术

The origin and evolution of V-rich, magnetite dominated Fe-Ti oxide mineralization; Northwest River Anorthosite, south-central Labrador, Canada

Published:2019-06-04 Issue:3 Volume:55 Page:555-575
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Valvasori Anthony A.,Hanchar John M.^ORCID,Piercey Stephen J.,Fonkwe Merline L. D.

Funder

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Research and Development Corporation of Newfoundland and Labrador

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-019-00892-6.pdf

Reference66 articles.

1. Ashwal LD (1982) Mineralogy of mafic and Fe-Ti oxide-rich differentiates of the Marcy anorthosite massif, Adirondacks, New York. Am Mineral 67:14–27

2. Ashwal LD (1993) Anorthosites. Spinger-Verlag, Berlin, p 422

3. Ashwal LD (2010) The temporality of anorthosites. Can Mineral 48:711–728

4. Augland LE, Moukhsil A, Solgadi F, Indares A (2015) Pinwarian to Grenvillian magmatic evolution in the central Grenville Province: new constraints from ID-TIMS U-Pb ages and coupled Lu-Hf S-MC-ICP-MS data. Can J Earth Sci 52:701–721

5. Bowles JF (1977) A method of tracing the temperature and oxygen-fugacity histories of complex magnetite-ilmenite grains. Mineral Mag 41:103–109

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