Nature of the lithospheric mantle beneath the Arabian Shield and genesis of Al-spinel micropods: Evidence from the mantle xenoliths of Harrat Kishb, Western Saudi Arabia
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文摘

Cr-diopside lherzolite and Al-augite wehrlite mantle xenolith types were described.

Former type is mostly mantle residue; while the latter one is deep mantle cumulate.

Peculiar Al-spinel micropods described for the first time from the wehrlite xenoliths.

Thermal and oxidation states beneath the Arabian Shield are inferred.

Genesis of Al-spinel micropods is discussed and compared with ophiolitic chromitite.

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