Cumulate xenoliths from Mt. Overlord, northern Victoria Land, Antarctica: A window into high pressure storage and differentiation of mantle-derived basalts
Mount Overlord (Antarctica) ultramafic xenolith mineral and whole rock study The samples represent high pressure cumulates related to Cenozoic magmatism. High pressure accumulation and differentiation of hydrous mantle derived melts Wet and hot deep zone in the Mount Overlord lithosphere