Element composition in various minerlas of ODP Hole 209-1274A peridotites, Mid-Atlantic
ODP Leg 209 Site 1274 mantle peridotites are highly refractory in terms of lack of residual clinopyroxene, olivine Mg# (up to 0.92) and spinel Cr# (~0.5), suggesting high degree of partial melting (>20%). Detailed studies of their microstructures show that they have extensively reacted with a per...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2007
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.668588 https://doi.org/10.1594/PANGAEA.668588 |