Contrasting types of chromium-spinel peridotite xenoliths in basanitic lavas, western Grand Canyon, Arizona-Reference-Cited by-同舟云学术

Contrasting types of chromium-spinel peridotite xenoliths in basanitic lavas, western Grand Canyon, Arizona

Published:1974-09 Issue:2 Volume:23 Page:229-237
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Best M.G.

Publisher

Elsevier BV

Subject

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

Reference25 articles.

1. Regional petrology of peridotite inclusions and basaltic host rocks;Forbes,1965

2. Al-augite and Cr-diopside ultramafic xenoliths in basaltic rocks from western United States: structural and textural relationships;Wilshire;Phys. Chem. Earth,1974

3. Chemistry of ultramafic nodules and their bearing on the origin of basaltic magmas;Kuno;Phys. Earth Planet. Interiors,1970

4. Plutonic xenoliths and their relation to the upper mantle;Harris;Phil. Trans. R. Soc. London,1972

5. Kaersutite-peridotite inclusions and kindred megacrysts in basanitic lavas, Grand Canyon, Arizona;Best;Contr. Mineral. Petrol.,1970

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