Timing and tectonic implications of the Pan-African Bangangte syenomonzonite, West Cameroon: Constraints from in-situ zircon U-Pb age and Hf-O isotopes
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文摘

Bangangte syenomonzonites in West Cameroon are emplaced at ∼584 Ma.

They are typical shoshonitic rocks generated by partial melting of an enriched mantle source.

These rocks display a transitional feature of subduction-related and within-plate shoshonites.

They emplaced in a post-collisional setting at the waning stage of Pan-African collisional orogeny.

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