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Ophiolites and Their Origins INTRODUCTION Ophiolites are the remnants of ancient oceanic crust and upper mantle that were tectonically emplaced into continental margins They display the only

Suprasubduction-zone ophiolites: Is there - ResearchGate

Ophiolites characterized by lavas with MORB geochemistry are typi- cally disrupted and found as fragments in accretionary complexes (e g , Franciscan), in contrast to suprasubduction-zone ophiolites

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Suprasubduction-zone ophiolites: Is there - ResearchGate