Reply to the comment of rollinson and adetunji “podiform chromitites do form beneath mid-ocean ridges” by Arai, S. And Miura, M

Author:

Arai Shoji,Miura Makoto

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference30 articles.

1. Petrology of podiform chromitite from the ocean floor at the 15°20’N FZ in the MAR, site 1271, ODP leg 209;Abe;Journal of Mineralogical and Petrological Sciences,2011

2. Behavior of MORB magmas at uppermost mantle beneath a fast-spreading axis: an example from wadi fizh of the Northern Oman ophiolite;Akizawa;Contributions to Mineralogy and Petrology,2012

3. Control of wall-rock composition on the formation of podiform chromitites as a result of magma/peridotite interaction;Arai;Resource Geology,1997

4. Podiform chromitites of the tari-misaka ultramafic complex, Southwestern Japan, as mantle-melt interaction products;Arai;Economic Geology,1994

5. Reaction of orthopyroxene in peridotite xenoliths with alkali basalt melt and its implication for genesis of alpine-type chromitite;Arai;American Mineralogist,1995

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