Ancient Melting Residual Peridotites Producing Variable Source Mantle beneath Mid-ocean Ridges: Detection and Geodynamic Implications-Reference-Cited by-同舟云学术

Ancient Melting Residual Peridotites Producing Variable Source Mantle beneath Mid-ocean Ridges: Detection and Geodynamic Implications

Published:2015 Issue:3 Volume:124 Page:333-354
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:Journal of Geography(Chigaku Zasshi)

Author:

MORISHITA Tomoaki¹

Affiliation:

1. School of Natural System, College of Science and Engineering, Kanazawa University

Publisher

Tokyo Geographical Society

Subject

Materials Chemistry

Link

https://www.jstage.jst.go.jp/article/jgeography/124/3/124_124.333/_pdf

Reference132 articles.

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2. Alard, O., Luguet, A., Pearson, J., Griffin, W.L., Lorand, J.-P., Gannoun, A., Burton, K.W. and O'Reilly, S.Y. (2005): In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle. Nature, 436, 1005-1008, doi:10.1038/nature03902.

3. Arai, S. (1987): An estimation of the least depleted spinel peridotite on the basis of olivine-spinel array. Neues Jahrbuch für Mineralogie-Monatshefte, 1987, 347-354.

4. Arai, S. (1992): Petrology of peridotites as a tool of insight into mantle processes: a review. Journal of Mineralogy, Petrology and Economic Geology, 87, 351-363.

5. Arai, S. (1994): Characterization of spinel peridotites by olivine-spinel compositional relationships: review and interpretation. Chemical Geology, 113, 191-204.

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