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Plate convergence usually commences with intra-oceanic Subduction, Andean margins commonly start after ophiolite obduct

Plate convergence usually commences with intra-oceanic Subduction, Andean margins commonly start after ophiolite obduction and subduction flip. CONVERGENT PLATE MARGINS Intra-oceanic (ensimatic) subduction Andean margins 3) Continent - continent collision zones. 1). 2). 3).

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