Origin of mantle peridotite: Constraints from melting experiments to 16.5 GPa

Author:

Herzberg Claude,Gasparik Tibor,Sawamoto Hiroshi

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference64 articles.

1. Mass balance and phase density constraints on early differentiation of chondritic mantle;Agee;Earth Planet. Sci. Lett.,1988

2. Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12-Mg3Al2Si3O12 and Fe4Si4O12-Fe3Al2Si3O12 at high pressures and temperatures;Akaogi;Phys. Earth Planet. Inter.,1977

3. Solar-system abundances of the elements;Anders;Geochim. Cosmochim. Acta,1982

4. Composition of the Earth;Anderson;Science,1989

5. High- and low-temperature garnet peridotite xenoliths and their possible relation to the lithosphere-asthenosphere boundary beneath southern Africa;Boyd,1987

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