Petrogenesis and tectonic implications of Triassic mafic complexes with MORB/OIB affinities from the western Garzê-Litang ophiolitic mélange, central Tibetan Plateau
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文摘

We report Triassic mafic complexes with MORB/OIB affinities from the western Garzê-Litang ophiolitic mélange (central Tibetan Plateau).

Geochemical and Sr-Nd isotopic data reveal that these rocks were likely derived from depleted MORB-type mantle metasomatized by crustal components or enriched lithospheric mantle metasomatized by OIB-like components.

We propose that a new model involving back-arc basin spreading associated with OIB/seamount recycling could account for geochemical variations of these rocks.

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