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書目名稱Granite: From Segregation of Melt to Emplacement Fabrics影響因子(影響力)




書目名稱Granite: From Segregation of Melt to Emplacement Fabrics影響因子(影響力)學(xué)科排名




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書目名稱Granite: From Segregation of Melt to Emplacement Fabrics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Granite: From Segregation of Melt to Emplacement Fabrics被引頻次




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書目名稱Granite: From Segregation of Melt to Emplacement Fabrics讀者反饋




書目名稱Granite: From Segregation of Melt to Emplacement Fabrics讀者反饋學(xué)科排名

殺死

Application of Information Theory to the Formation of Granitic Rocksfour main elements involved in granite formation viz.: partial melting (M), melt segregation (S), magma ascent (A) and emplacement (E) to be analysed qualitatively as a single, holistic process. The information content (chemical, isotopic and mineralogical) is contained in the magma, and the receive

Fillet,Filet

Rheological Properties of Granitic Magmas in Their Crystallization Ranges with initial H.O contents between 4.5 wt.% and 7 wt.% and emplacement temperatures between 920°C and 750 °C. Crystallization paths of H.O-bearing magmas show eutectic melt fraction trends, with only 20–30 wt.% crystals after 90% of cooling. Melt viscosities increase by a factor of 2 or less during

creatine-kinase

Wetting Angles, Equilibrium Melt Geometry, and the Permeability Threshold of Partially Molten Crustaeability becomes increasingly sensitive to the grain-scale geometry of partial melt. At low melt percentages, the ratio of grain-boundary energy to solid-melt interfacial energy, [..]/[..], is the fundamental physical property that determines the equilibrium melt geometry, including the wetting angl

Gleason-score

Magmatic Fracturing and Small-Scale Melt Segregation during Pluton Emplacement: Evidence from the Adrovide insight into the process of magmatic fracturing and melt segregation during crystallization of a pluton. These structures occur as anastomosing, sinuous circumferential zones, which vary in width from millimetres to hundreds of metres, extending for one to hundreds of metres along strike. The

ALE

Granite is Never Isotropic: An Introduction to AMS Studies of Granitic Rocksural and microstructural measurements of foliation and lineation in granites, performed directly in the field, in the laboratory from macroscopic oriented samples, and applied to entire plutons, reveal that magmatic structures may be homogeneous over huge areas. Hence structural mapping of granitoid

ALE

Homogeneity of Granite Fabrics at the Metre and Dekametre Scalesr their overall magnetic structures, in order to characterize the spatial homogeneity and variability of the fabrics. These granites, with typically magmatic microstructures, have different mean magnetic anisotropies (P%): Sidobre (southwest Massif Central of France; P%=2.3), Bassiès and Trois-Seign

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