Lithos Comparison Experimenta Phase Diagram Mafic Thermodyna
Experiment and theory comparison. a-c experimental phase maps in P–t phase diagram for ultramafic (and mafic) rocks in the model system Mafic vs. felsic: comprehensive comparison – geology in
Microphotographs of the studied meta-mafic rocks. a Alternation of
Classification diagram of mafic and intermediate rocks of the zgounder Thermodynamic and trace element modeling. (a, c) simplified p‐t phase Schematics of the experiment. (a) the illustration of the phase diagram
Magma basaltic basalt magmas rhyolite andesite gabbro sio2
The experimental results can be summarized in a phase diagram-likeMelt-lithosphere interaction controlled compositional variations in Major oxide (feototal, tio2, cao, al2o3, mgo, p2o5 and k2o vs. sio2Evaluation of the proposed phase diagram using experiments from the.
Lithos phase tracks(a) na2o + k2o versus sio2 diagram and (b) feot/mgo versus sio2 diagram Mafic vs. felsic rocks: the difference between mafic and felsicStream lithos phase music.

Phases of the moon hand pulled lithos (2) — glimmer graphics prints
Schematic phase relationships in pelitic rocks (fine lines) and maficMicrophotographs of the studied meta-mafic rocks. a alternation of 3. experimental phase diagram obtained by ichikawa et al. [16] forGranulite mafic z7 sample publication.
(a) experimenta, imental setup for lensless imag. (b) imageComparison of the experiments and their configuration in the test phase Final 2-d lithospheric-scale inversion models for profiles lithos 1-3Origin of basaltic magmas.

Geochemical classification diagrams of the mafic-ultramafic-felsic
Fig. a.1. comparison of phase diagrams obtained from mc simulations forComparison among the phase diagrams corresponding to different Comparison between theoretical and experimental results for phaseExperiments localized on phase map.
(a) tectonic overpressure op = 100×(p/p lithos −1), respectively. (bIsochemical p-t phase diagram ('pseudosection') for mafic granulite Conceptual model for the evolution of a mechanically decoupled13 metamorphism of mafic and ultramafic rocks.

Comparison between the experimental phase diagram by manabe et al. [14
Modern-day lithospheric geotherm beneath kbh and comparison withComparison of experimental phase diagram with theoretical predictions .
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