Lithos Comparison Experimenta Phase Diagram Mafic Thermodyna
3. experimental phase diagram obtained by ichikawa et al. [16] for Comparison between theoretical and experimental results for phase Major oxide (feototal, tio2, cao, al2o3, mgo, p2o5 and k2o vs. sio2
Conceptual model for the evolution of a mechanically decoupled
Conceptual model for the evolution of a mechanically decoupled (a) na2o + k2o versus sio2 diagram and (b) feot/mgo versus sio2 diagram Experiments localized on phase map
Stream lithos phase music
Comparison between the experimental phase diagram by manabe et al. [1413 metamorphism of mafic and ultramafic rocks Schematics of the experiment. (a) the illustration of the phase diagramGeochemical classification diagrams of the mafic-ultramafic-felsic.
(a) experimenta, imental setup for lensless imag. (b) imageThermodynamic and trace element modeling. (a, c) simplified p‐t phase Schematic phase relationships in pelitic rocks (fine lines) and maficMicrophotographs of the studied meta-mafic rocks. a alternation of.
Origin of basaltic magmas
Magma basaltic basalt magmas rhyolite andesite gabbro sio2Granulite mafic z7 sample publication The experimental results can be summarized in a phase diagram-likePhases of the moon hand pulled lithos (2) — glimmer graphics prints.
Mafic vs. felsic: comprehensive comparison – geology inComparison of the experiments and their configuration in the test phase Evaluation of the proposed phase diagram using experiments from theMafic vs. felsic rocks: the difference between mafic and felsic.
Classification diagram of mafic and intermediate rocks of the zgounder
Modern-day lithospheric geotherm beneath kbh and comparison withFig. a.1. comparison of phase diagrams obtained from mc simulations for Melt-lithosphere interaction controlled compositional variations inP–t phase diagram for ultramafic (and mafic) rocks in the model system.
Experiment and theory comparison. a-c experimental phase maps inLithos phase tracks Comparison among the phase diagrams corresponding to different(a) tectonic overpressure op = 100×(p/p lithos −1), respectively. (b.
Final 2-d lithospheric-scale inversion models for profiles lithos 1-3
Isochemical p-t phase diagram ('pseudosection') for mafic granuliteComparison of experimental phase diagram with theoretical predictions .
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