Absence of molybdenum isotope fractionation during magmatic differentiation at Hekla volcano, Iceland-Reference-Cited by-同舟云学术

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Absence of molybdenum isotope fractionation during magmatic differentiation at Hekla volcano, Iceland

Published:2015-08 Issue: Volume:162 Page:126-136
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Yang Jie,Siebert Christopher,Barling Jane,Savage Paul,Liang Yu-Hsuan,Halliday Alex N.

Funder

University of Oxford

St Anne's College, Oxford

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference71 articles.

1. Molybdenum stable isotopes: Observations, interpretations and directions;Anbar;Rev. Mineral. Geochem.,2004

2. Distribution of major and minor elements in coexisting minerals from a metamorphosed iron formation;Annersten;Lithos,1971

3. The isotopic signature of the global riverine molybdenum flux and anoxia in the ancient oceans;Archer;Nat. Geosci.,2008

4. Source and evolution of molybdenum in the porphyry Mo(-Nb) deposit at Cave Peak, Texas;Audétat;J. Petrol.,2010

5. Magmatic evolution of Hekla, Iceland;Baldridge;Contrib. Miner. Petrol.,1973

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