A melting model for variably depleted and enriched lherzolite in the plagioclase and spinel stability fields
Here we develop a lherzolite melting model and explore the effects of variations in mantle composition, pressure, temperature, and H[subscript 2]O content on melt composition. New experiments and a compilation of experimental liquids saturated with all of the mantle minerals (olivine, orthopyroxene,...
| Main Authors: | , , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union (AGU)
2012
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| Online Access: | http://hdl.handle.net/1721.1/74032 https://orcid.org/0000-0003-3136-4942 |