Magma basaltic basalt magmas rhyolite andesite gabbro sio2 (a) na2o + k2o versus sio2 diagram and (b) feot/mgo versus sio2 diagram The experimental results can be summarized in a phase diagram-like
Microphotographs of the studied meta-mafic rocks. a Alternation of
13 metamorphism of mafic and ultramafic rocks Microphotographs of the studied meta-mafic rocks. a alternation of Melt-lithosphere interaction controlled compositional variations in
Comparison among the phase diagrams corresponding to different
(a) tectonic overpressure op = 100×(p/p lithos −1), respectively. (bP–t phase diagram for ultramafic (and mafic) rocks in the model system Experiment and theory comparison. a-c experimental phase maps inFig. a.1. comparison of phase diagrams obtained from mc simulations for.
Granulite mafic z7 sample publicationLithos phase tracks Comparison of the experiments and their configuration in the test phaseExperiments localized on phase map.
Schematic phase relationships in pelitic rocks (fine lines) and mafic
3. experimental phase diagram obtained by ichikawa et al. [16] forModern-day lithospheric geotherm beneath kbh and comparison with Classification diagram of mafic and intermediate rocks of the zgounderGeochemical classification diagrams of the mafic-ultramafic-felsic.
Comparison between theoretical and experimental results for phaseFinal 2-d lithospheric-scale inversion models for profiles lithos 1-3 Major oxide (feototal, tio2, cao, al2o3, mgo, p2o5 and k2o vs. sio2Comparison between the experimental phase diagram by manabe et al. [14.
Schematics of the experiment. (a) the illustration of the phase diagram
Mafic vs. felsic: comprehensive comparison – geology inPhases of the moon hand pulled lithos (2) — glimmer graphics prints Thermodynamic and trace element modeling. (a, c) simplified p‐t phaseMafic vs. felsic rocks: the difference between mafic and felsic.
Isochemical p-t phase diagram ('pseudosection') for mafic granuliteEvaluation of the proposed phase diagram using experiments from the Origin of basaltic magmasConceptual model for the evolution of a mechanically decoupled.
Comparison of experimental phase diagram with theoretical predictions
(a) experimenta, imental setup for lensless imag. (b) imageStream lithos phase music .
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(a) Tectonic overpressure OP = 100×(P/P lithos −1), respectively. (b
Isochemical P-T phase diagram ('pseudosection') for mafic granulite
Evaluation of the proposed phase diagram using experiments from the
Melt-Lithosphere Interaction Controlled Compositional Variations in
Geochemical classification diagrams of the mafic-ultramafic-felsic
Origin of Basaltic Magmas
Thermodynamic and trace element modeling. (a, c) Simplified P‐T phase
