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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
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書目名稱Granite: From Segregation of Melt to Emplacement Fabrics被引頻次學(xué)科排名
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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
作者: 殺死 時間: 2025-3-21 23:22
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作者: Fillet,Filet 時間: 2025-3-22 02:23
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作者: creatine-kinase 時間: 2025-3-22 04:55
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作者: Gleason-score 時間: 2025-3-22 09:25
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作者: ALE 時間: 2025-3-22 16:20
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作者: ALE 時間: 2025-3-22 18:37
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作者: 勾引 時間: 2025-3-22 22:56 作者: 吞沒 時間: 2025-3-23 03:59 作者: PHAG 時間: 2025-3-23 09:32 作者: MANIA 時間: 2025-3-23 12:27 作者: 喚起 時間: 2025-3-23 16:42 作者: 蓋他為秘密 時間: 2025-3-23 18:06 作者: 類人猿 時間: 2025-3-24 01:16 作者: 翻布尋找 時間: 2025-3-24 02:44 作者: PRO 時間: 2025-3-24 08:31 作者: BLAND 時間: 2025-3-24 11:55
Parul Pant,Aadya Jaipuria,Chetna Guptafour 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作者: Alveolar-Bone 時間: 2025-3-24 17:05
Ram R. R. Prasad,Qian Jia,Paul A. Wrights 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作者: BORE 時間: 2025-3-24 19:42 作者: Dictation 時間: 2025-3-25 01:35 作者: Nefarious 時間: 2025-3-25 05:40
https://doi.org/10.1007/978-3-7091-5947-7ural 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作者: 牌帶來 時間: 2025-3-25 10:38
https://doi.org/10.1007/3-540-34011-4r 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作者: MUTE 時間: 2025-3-25 12:22 作者: DRILL 時間: 2025-3-25 17:12 作者: 凝乳 時間: 2025-3-25 22:11
https://doi.org/10.1007/978-3-7091-5946-0ultz-sous-Forêt, France, are described and interpreted. Preferred orientations of biotite (001) planes and feldspar (010) and (100) cleavages, were measured by means of an optical goniometer. The poles of (001) biotites show stable orientations throughout the core with maximum eigenvector v oriented作者: 消毒 時間: 2025-3-26 01:40
Glühlicht, Funkenlegierungen, Leuchtsteines of Shape Preferred Orientations (SPO) of crystals in igneous rocks. A classical result of the theoretical model is that the SPO should rotate and pulsate with increasing strain, with a periodicity equal to that of the rotation of an individual particle. However, the initial theoretical model makes作者: 憤慨一下 時間: 2025-3-26 05:50 作者: LINE 時間: 2025-3-26 12:05 作者: 外面 時間: 2025-3-26 13:06
Herbert Wiemann,Ulrich Eberle,Alfred Soherric rocks of the Central Iberian Zone. The LPB is composed of granodiorites, a dyke swarm, and granites emplaced during three successive magmatic events. Field structural data from both the country rocks and the LPB indicate that the northern boundary of the LPB is a transtensional shear zone, the Co作者: 牲畜欄 時間: 2025-3-26 19:16 作者: 配置 時間: 2025-3-26 23:37
https://doi.org/10.1007/978-3-642-51334-3ostructural observations are combined with an AMS study of 172 stations. The continuum between charnockites and granites is revealed by their constituent minerals and the magnetic susceptibility map. The contemporaneity of emplacement of all the petrographic types is demonstrated by their similar mi作者: Acquired 時間: 2025-3-27 01:11
Parul Pant,Aadya Jaipuria,Chetna Guptabe expressed symbolically as:.where . and Λ represent information loss by noise and weathering, counteracted by redundancy . and input from the investigators δ. The processes involved in granitoid formation, as identified by the application of information theory, are likely to be cyclic. By defining作者: MANIA 時間: 2025-3-27 07:52 作者: eucalyptus 時間: 2025-3-27 12:24 作者: 正面 時間: 2025-3-27 14:27
What Does the Histology Tell Us?walls. The shortening direction remained constant throughout emplacement..If, at low melt fractions, melt pressure exceeds cohesion along the foliation, fractures can open normal to the shortening direction. Alternatively, dikes may also form as shear fractures parallel to the plane of anisotropy (a作者: critic 時間: 2025-3-27 19:25 作者: Fatten 時間: 2025-3-27 23:16 作者: Consequence 時間: 2025-3-28 03:45
Strukturelle Phasenumwandlungen,t rotate as much and deviates 10° from that expected. For larger shear strains, the fabrics are consistently oriented, but a 10° offshear-plane deviation remains. From these experiments we conclude that, even at low concentrations of crystals, magmatic biotite subfabrics are not expected to behave c作者: Landlocked 時間: 2025-3-28 07:07
https://doi.org/10.1007/978-3-7091-5946-0etry in these sections. Numerical modelling involving a component of coaxial flattening, with various amounts of extension parallel and perpendicular to stretch, in addition to simple shearing, agrees qualitatively with the observed data. The models demonstrate that, under combined coaxial and simpl作者: 樂章 時間: 2025-3-28 13:18 作者: 存心 時間: 2025-3-28 18:09 作者: Enthralling 時間: 2025-3-28 22:40 作者: indices 時間: 2025-3-29 02:54
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作者: Immortal 時間: 2025-3-29 03:37 作者: 制度 時間: 2025-3-29 11:15
Rheological Aspects of Magma Transport Inferred from Rock Structures作者: ARM 時間: 2025-3-29 11:46
Granite: From Segregation of Melt to Emplacement Fabrics作者: Ligneous 時間: 2025-3-29 18:47 作者: 苦澀 時間: 2025-3-29 22:57
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作者: 大火 時間: 2025-3-30 01:59
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作者: Tdd526 時間: 2025-3-30 04:06 作者: 極小 時間: 2025-3-30 10:21 作者: 終點 時間: 2025-3-30 16:11
Homogeneity of Granite Fabrics at the Metre and Dekametre Scales such as a C/S system was observed. The magnetic anisotropy and the bulk susceptibility are homogeneous as a whole, and display spatial organizations with no simple relationships with the structures. These results confirm, however, the validity of the homogeneous structural patterns obtained from en作者: comely 時間: 2025-3-30 16:40
Analogue 3D Simple-Shear Experiments of Magmatic Biotite Subfabricst rotate as much and deviates 10° from that expected. For larger shear strains, the fabrics are consistently oriented, but a 10° offshear-plane deviation remains. From these experiments we conclude that, even at low concentrations of crystals, magmatic biotite subfabrics are not expected to behave c作者: GROG 時間: 2025-3-31 00:11 作者: Interferons 時間: 2025-3-31 04:47
Rigid Particles in Simple Shear Flow: Is Their Preferred Orientation Periodic or Steady-State ?/matrix interface may not always be coherent; and (iii) the aspect ratios of the crystals defining the SPO are unlikely to be unique and constant, as assumed in the model. The last point is discussed on the basis of some 2D simple calculations of the development of SPO defined by different types of 作者: 后來 時間: 2025-3-31 09:00 作者: 無法取消 時間: 2025-3-31 10:30
Granite Pluton Geometry and Emplacement Mode Inferred from Combined Fabric and Gravity Datafeeder zones. They are emplaced as sills in the upper crust, or within rather ductile environments in extensionnal tectonic contexts. These contrast with the thick (more than 10 kilometres) wedge-shaped plutons, extending largely in one direction along which a few root zones appear, which are V-shap作者: Solace 時間: 2025-3-31 14:50 作者: 帶傷害 時間: 2025-3-31 21:29
Development of Magmatic to Solid-State Fabrics during Syntectonic Emplacement of the Mono Creek Granprovide semi-quantitative information: K correlates with rock mineralogy, and P is a good indicator of the rock texture. The AMS directional data of the MCG are characterized by good clustering at each sampling station, and by a sigmoidal pattern of foliation and lineation. This pattern results from作者: Vo2-Max 時間: 2025-3-31 22:59 作者: 粗魯性質(zhì) 時間: 2025-4-1 05:08
https://doi.org/10.1007/978-3-642-51334-3r zones were responsible for the migration, drainage and tapping of magmas from the source region. The inclined attitude of the shear zones would have acted as a roof-guide for the up-rising magmas. Finally, the transcurrent movement most likely enhanced the upward migration of magmas.
