存心
发表于 2025-3-28 18:09:33
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Enthralling
发表于 2025-3-28 22:40:40
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indices
发表于 2025-3-29 02:54:24
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
发表于 2025-3-29 03:37:14
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制度
发表于 2025-3-29 11:15:23
Rheological Aspects of Magma Transport Inferred from Rock Structures
ARM
发表于 2025-3-29 11:46:06
Granite: From Segregation of Melt to Emplacement Fabrics
Ligneous
发表于 2025-3-29 18:47:30
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苦涩
发表于 2025-3-29 22:57:58
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
发表于 2025-3-30 01:59:29
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
发表于 2025-3-30 04:06:43
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