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Ultra-refractory mantle within oceanic plateau: Petrology of the spinel harzburgites from Lac Michèle, Kerguelen Archipelago
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文摘
Spinel harzburgites from Lac Michèle are the most refractory peridotites within ocean LIP. They are formed by > 30% of fractional polybaric partial melting at 5 –≤ 1 GPa. They have modal, major and trace element composition similar to on-craton peridotites.

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