Water–rock interactions, orthopyroxene growth, and Si-enrichment in the mantle: evidence in xenoliths from the Colorado Plateau, southwestern United States-Reference-Cited by-同舟云学术

Water–rock interactions, orthopyroxene growth, and Si-enrichment in the mantle: evidence in xenoliths from the Colorado Plateau, southwestern United States

Published:1999-01 Issue:1 Volume:165 Page:45-54
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Smith Douglas,Alexis Riter J.C.,Mertzman Stanley A.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference35 articles.

1. D. Smith, Hydrous minerals and carbonates in peridotite inclusions from the Green Knobs and Buell Park kimberlitic diatremes on the Colorado Plateau, in: F.R. Boyd, H.O.A. Meyer (Eds.), Proc. 2nd International Kimberlite Conf. 2, American Geophysical Union, Washington, D.C., 1979, pp. 345–356.

2. H. Helmstaedt, D.J. Schulze, Garnet clinopyroxenite–chlorite eclogite transition in a xenolith from Moses Rock: further evidence for metamorphosed ophiolites under the Colorado Plateau, in: F.R. Boyd, H.O.A. Meyer (Eds.), Proc. 2nd International Kimberlite Conf. 2, American Geophysical Union, Washington, D.C., 1979, pp. 357–365.

3. Genesis and evolution of low-Al orthopyroxene in spinel peridotite xenoliths, Grand Canyon field, Arizona, USA;Smith;Contrib. Mineral. Petrol.,1997

4. Peridotite xenoliths from western Grand Canyon and The Thumb: A probe into the subcontinental mantle of the Colorado Plateau;Alibert;J. Geophys. Res.,1994

5. Fluids in equilibrium with peridotite minerals: implications for mantle metasomatism;Schneider;Geochim. Cosmochim. Acta,1986

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