Reactive Melt Flow as the Origin of Residual Mantle Lithologies and Basalt Chemistries in Mid-Ocean Ridges: Implications from the Red Hills Peridotite, New Zealand-Reference-Cited by-同舟云学术

Reactive Melt Flow as the Origin of Residual Mantle Lithologies and Basalt Chemistries in Mid-Ocean Ridges: Implications from the Red Hills Peridotite, New Zealand

Published:2012-05-07 Issue:8 Volume:53 Page:1637-1671
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:Journal of Petrology

Author:

Kimura J.-I.,Sano S.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/53/8/1637/4263038/egs028.pdf

Reference81 articles.

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2. A model that reconciles major- and trace-element data from abyssal peridotites

3. Steady-state Mantle-Melt Interactions in One Dimension: I. Equilibrium Transport and Melt Focusing

4. Evolution of LILE-enriched small melt fractions in the lithospheric mantle: a case study from the East African Rift

5. Lithostratigraphy and structure of the Caples terrane of the Humboldt Mountains, New Zealand

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