Titlebook: ;

存心

Enthralling

indices

Herbert Wiemann,Ulrich Eberle,Alfred Soherrthe LPB was controlled by a crustal scale and dextral transtensional shear zone, parallel to the batholith elongation. The eastern part of the granodiorite takes the shape of a large laccolith prolonged westwards by four NW-SE elongate domes. These contrasted geometries reflect the upwelling of magm

Immortal

制度

Rheological Aspects of Magma Transport Inferred from Rock Structures

ARM

Granite: From Segregation of Melt to Emplacement Fabrics

Ligneous

苦澀

Rheological Properties of Granitic Magmas in Their Crystallization Rangewering effect of H.O upon viscosity, except at very low fluid/melt mass ratios. As a consequence, magma viscosities of H.O-CO.-bearing magmas may increase much more rapidly during crystallization, in some instances by many orders of magnitude relative to H.O-bearing magmas. Phase equilibrium results

大火

Wetting Angles, Equilibrium Melt Geometry, and the Permeability Threshold of Partially Molten Crustatural systems where solid-melt interfacial energies are essentially anisotropic..Measurements of wetting angles at quartz-quartz-melt, feldspar-feldspar-melt and amphibole-amphibole-melt triple junctions consistently yielded low to very low median values, in the range 10°–60°. These low angles resul

Tdd526