Are Variations in TiO2 Contents in Anorthite-Hosted MORB Melt Inclusions Controlled by Magma Compositions or Boundary Layer Phenomena?

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ADS bibcode: 2007AGUFM.V11B0587W
year: 2007
Listed Authors: Weinsteiger, A. B.; Kent, A. J.; Nielsen, R. L.; Tepley, F. J.
Listed Institutions: Oregon State University Department of Geosciences, 104 Wilkinson Hall, Corvallis, 0R 97331, United States; Oregon State University Department of Geosciences, 104 Wilkinson Hall, Corvallis, 0R 97331, United States; Oregon State University Department of Geosciences, 104 Wilkinson Hall, Corvallis, 0R 97331, United States; Oregon State University Department of Geosciences, 104 Wilkinson Hall, Corvallis, 0R 97331, United States

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Oregon State University, Corvallis