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Classification diagram of mafic and intermediate rocks of the zgounder
Schematic phase relationships in pelitic rocks (fine lines) and mafic(a) tectonic overpressure op = 100×(p/p lithos −1), respectively. (b Magma basaltic basalt magmas rhyolite andesite gabbro sio2Conceptual model for the evolution of a mechanically decoupled.
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Experiment and theory comparison. a-c Experimental phase maps in
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Mafic Vs. Felsic Rocks: The Difference Between Mafic and Felsic
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Fig. A.1. Comparison of phase diagrams obtained from MC simulations for
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Geochemical classification diagrams of the mafic-ultramafic-felsic
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Conceptual model for the evolution of a mechanically decoupled