Polymineral-Metasomatic Crystallogenesis [electronic resource] / by Arkady E. Glikin.

By: Glikin, Arkady E [author.]Contributor(s): SpringerLink (Online service)Material type: TextTextPublisher: Dordrecht : Springer Netherlands, 2009Description: XIV, 312 p. online resourceContent type: text Media type: computer Carrier type: online resourceISBN: 9781402089831Subject(s): Physics | Inorganic chemistry | Geochemistry | Mineralogy | Crystallography | Physics | Crystallography | Inorganic Chemistry | Geochemistry | MineralogyAdditional physical formats: Printed edition:: No titleDDC classification: 548 LOC classification: QD901-999Online resources: Click here to access online
Contents:
Replacement of Monocrystals -- Joint Growth of Crystals of Different Phases -- Formation of Mixed Crystals in Solutions -- Physicochemical Analysis of Metasomatic Crystallogenesis -- Metasomatic Transformation of Aggregates -- Epitaxy and Quasiepitaxy in Solutions -- Crystal Faceting.
In: Springer eBooksSummary: Polymineral-Metasomatic Crystallogenesis is dedicated to the foundations of polymineral crystallogenesis in solutions typically occurring in nature. Effects, laws, and mechanisms of a metasomatic crystal replacement, joint crystal growth of different phases, mixed crystal formation, and aggregate re-crystallization as well as oriented overgrowth (epitaxy and quasi-epitaxy) and crystal habit origin are considered experimentally. The behaviour of these processes in nature are discussed in addition to pseudomorphs, poikilitic crystals (and other replacement forms), features of rapakivi structure, fluorite morphology, and many more. The concept is a generalization of the classic theory on crystallogenesis which is complicated by phase interaction in polymineral systems. Polymineral-Metasomatic Crystallogenesis is designed for chemists, geologists, physicists, and postgraduates and advanced undergraduate students of these fields.
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Replacement of Monocrystals -- Joint Growth of Crystals of Different Phases -- Formation of Mixed Crystals in Solutions -- Physicochemical Analysis of Metasomatic Crystallogenesis -- Metasomatic Transformation of Aggregates -- Epitaxy and Quasiepitaxy in Solutions -- Crystal Faceting.

Polymineral-Metasomatic Crystallogenesis is dedicated to the foundations of polymineral crystallogenesis in solutions typically occurring in nature. Effects, laws, and mechanisms of a metasomatic crystal replacement, joint crystal growth of different phases, mixed crystal formation, and aggregate re-crystallization as well as oriented overgrowth (epitaxy and quasi-epitaxy) and crystal habit origin are considered experimentally. The behaviour of these processes in nature are discussed in addition to pseudomorphs, poikilitic crystals (and other replacement forms), features of rapakivi structure, fluorite morphology, and many more. The concept is a generalization of the classic theory on crystallogenesis which is complicated by phase interaction in polymineral systems. Polymineral-Metasomatic Crystallogenesis is designed for chemists, geologists, physicists, and postgraduates and advanced undergraduate students of these fields.

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