Deformation processes in mantle peridotites : with emphasis on the Ronda peridotite of SW Spain
This thesis aims to study upper mantle deformation processes in a case study of the Ronda peridotite in the Alpine Betic Cordilleras of SW Spain. The choice for this massif is motivated by its following characteristics: (i) pioneering geochemical and geological studies have shown that the W Mediterranean peridotites are among the most heterogeneous ...
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Genesis of Hawaiian lavas by crystallization of picritic magma in the deep mantle. [PDF]
Yang J, Wang C, Zhang J, Jin Z.
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Carbonates and intermediate-depth seismicity: Stable and unstable shear in altered subducting plates and overlying mantle. [PDF]
Prakash A+5 more
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Mexican Peridotite Xenoliths and Tectonic Terranes: Correlations among Vent Location, Texture, Temperature, Pressure, and Oxygen Fugacity [PDF]
James F. Luhr, José Jorge Aranda-Gómez
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Melt–Peridotite Reactions and Fluid Metasomatism in the Upper Mantle, Revealed from the Geochemistry of Peridotite and Gabbro from the Horoman Peridotite Massif, Japan [PDF]
Akio Makishima+2 more
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The evolution of the Galápagos mantle plume. [PDF]
Soderman CR+5 more
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Polybaric Petrogenesis of Mafic Layers in the Horoman Peridotite Complex, Japan [PDF]
Eiichi Takazawa+4 more
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Metamorphism of Venus as driver of crustal thickness and recycling. [PDF]
Semprich J+4 more
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Frictional melting mechanisms of rocks during earthquake fault slip. [PDF]
Woo S, Han R, Oohashi K.
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