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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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473 views • 19 slides

Grand Challenge: Why Does Volcanism Occur Where and When it Occurs in the Basin and Range?

Grand Challenge: Why Does Volcanism Occur Where and When it Occurs in the Basin and Range?. Richard W. Carlson Carnegie Institution of Washington Department of Terrestrial Magn(m)atism. EarthScope Great Breaks Workshop. June 22, 2004.

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272 views • 12 slides

A Levander et al. Nature 515 , 253-256 (2014) doi:10.1038/nature13878

Gibraltar arc region tectonic features, lithosphere thickness, positive P-wave tomography anomalies, and P-wave anomaly restored to the surface. A Levander et al. Nature 515 , 253-256 (2014) doi:10.1038/nature13878.

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78 views • 1 slides

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Lithosphere thickness - PowerPoint PPT Presentation

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

Grand Challenge: Why Does Volcanism Occur Where and When it Occurs in the Basin and Range?

A Levander et al. Nature 515 , 253-256 (2014) doi:10.1038/nature13878