Articles liés à Granite: From Segregation of Melt to Emplacement Fabrics
Synopsis
viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous "Granite Controversy" (1957). Read's formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opened era during which emerging an granites were considered mainly from this new viewpoint. Geochemical signatures have shown that mantle and crustal origins for granites were both possible, but the debate on how and why granites are emplaced did not progress much. Meanwhile, structural geology was essentially geometrical and mechanistic. In the early 70's, the structural approach began to widen to include solid state physics and fluid dynamics. Detailed structural maps of granitic bodies were again published, mainly in France, and analysed in terms of magmatic and plastic flow. The senior editor of this volume and his students deserve much of the credit for this new development. Via microstructural and petrofabric studies, they were able to discriminate between strain in the presence of residual melt or in the solid-state, and, by systematically measuring magnetic fabrics (AMS), they have been able to map magmatic foliations and lineations in ever finer detail, using the internal markers within granites coming from different tectonic environments. The traditional debate has been shifted anew. The burning question now seems to be how the necessary, large-scale or local, crustal extension required for granite emplacement can be obtained.
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Granite. From Segregation of Melt to Emplacement Fabrics
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Kluwer Academic, Dordrecht, 1997
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Granite: From Segregation of Melt to Emplacement Fabrics (Petrology and Structural Geology, 8)
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Granite: From Segregation of Melt to Emplacement Fabrics (Petrology and Structural Geology, 8)
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Granite: From Segregation of Melt to Emplacement Fabrics
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Gebunden. Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous Granite Controversy (1957). Read s formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opene. N° de réf. du vendeur 5968042
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Granite: From Segregation of Melt to Emplacement Fabrics
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Springer Netherlands Mrz 1997, 1997
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Buch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous 'Granite Controversy' (1957). Read's formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opened era during which emerging an granites were considered mainly from this new viewpoint. Geochemical signatures have shown that mantle and crustal origins for granites were both possible, but the debate on how and why granites are emplaced did not progress much. Meanwhile, structural geology was essentially geometrical and mechanistic. In the early 70's, the structural approach began to widen to include solid state physics and fluid dynamics. Detailed structural maps of granitic bodies were again published, mainly in France, and analysed in terms of magmatic and plastic flow. The senior editor of this volume and his students deserve much of the credit for this new development. Via microstructural and petrofabric studies, they were able to discriminate between strain in the presence of residual melt or in the solid-state, and, by systematically measuring magnetic fabrics (AMS), they have been able to map magmatic foliations and lineations in ever finer detail, using the internal markers within granites coming from different tectonic environments. The traditional debate has been shifted anew. The burning question now seems to be how the necessary, large-scale or local, crustal extension required for granite emplacement can be obtained. 372 pp. Englisch. N° de réf. du vendeur 9780792344605
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Granite
Edité par
Kluwer Academic Publishers, 1997
ISBN 10 : 079234460X
ISBN 13 : 9780792344605
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Vendeur : Kennys Bookshop and Art Galleries Ltd., Galway, GY, Irlande
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Etat : New. Granite is the most abundant rock on the continental crust, and this text is devoted to the understanding of its origins and emplacement by studying its internal structures. It covers a range of topics related to the physical aspects of granite magmatism. It is useful to geologists, petrologists, and geophysicists. Editor(s): Bouchez, Jean-Luc; Hutton, D.; Stephens, W. E. Series: Petrology and Structural Geology. Num Pages: 368 pages, biography. BIC Classification: RBGG; RBGL. Category: (P) Professional & Vocational. Dimension: 234 x 156 x 22. Weight in Grams: 698. . 1997. Hardback. . . . . N° de réf. du vendeur V9780792344605
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Granite
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Etat : New. pp. 372. N° de réf. du vendeur 263063009
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Granite: From Segregation of Melt to Emplacement Fabrics
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Springer Netherlands, Springer Netherlands Mär 1997, 1997
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ISBN 13 : 9780792344605
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Vendeur : buchversandmimpf2000, Emtmannsberg, BAYE, Allemagne
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Buch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous 'Granite Controversy' (1957). Read's formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opened era during which emerging an granites were considered mainly from this new viewpoint. Geochemical signatures have shown that mantle and crustal origins for granites were both possible, but the debate on how and why granites are emplaced did not progress much. Meanwhile, structural geology was essentially geometrical and mechanistic. In the early 70's, the structural approach began to widen to include solid state physics and fluid dynamics. Detailed structural maps of granitic bodies were again published, mainly in France, and analysed in terms of magmatic and plastic flow. The senior editor of this volume and his students deserve much of the credit for this new development. Via microstructural and petrofabric studies, they were able to discriminate between strain in the presence of residual melt or in the solid-state, and, by systematically measuring magnetic fabrics (AMS), they have been able to map magmatic foliations and lineations in ever finer detail, using the internal markers within granites coming from different tectonic environments. The traditional debate has been shifted anew. The burning question now seems to be how the necessary, large-scale or local, crustal extension required for granite emplacement can be obtained.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 372 pp. Englisch. N° de réf. du vendeur 9780792344605
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Granite
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Etat : New. Print on Demand pp. 372 52:B&W 6.14 x 9.21in or 234 x 156mm (Royal 8vo) Case Laminate on White w/Gloss Lam. N° de réf. du vendeur 5833534
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Granite: From Segregation of Melt to Emplacement Fabrics
Edité par
Springer Netherlands, Springer Netherlands, 1997
ISBN 10 : 079234460X
ISBN 13 : 9780792344605
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Vendeur : AHA-BUCH GmbH, Einbeck, Allemagne
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Buch. Etat : Neu. Druck auf Anfrage Neuware - Printed after ordering - viii debate of those earlier days has been beautifully summarized by H. H. Read in his famous 'Granite Controversy' (1957). Read's formulation of the controversy occurred at the time when geochemistry was as a new and powerful tool. The new techniques opened era during which emerging an granites were considered mainly from this new viewpoint. Geochemical signatures have shown that mantle and crustal origins for granites were both possible, but the debate on how and why granites are emplaced did not progress much. Meanwhile, structural geology was essentially geometrical and mechanistic. In the early 70's, the structural approach began to widen to include solid state physics and fluid dynamics. Detailed structural maps of granitic bodies were again published, mainly in France, and analysed in terms of magmatic and plastic flow. The senior editor of this volume and his students deserve much of the credit for this new development. Via microstructural and petrofabric studies, they were able to discriminate between strain in the presence of residual melt or in the solid-state, and, by systematically measuring magnetic fabrics (AMS), they have been able to map magmatic foliations and lineations in ever finer detail, using the internal markers within granites coming from different tectonic environments. The traditional debate has been shifted anew. The burning question now seems to be how the necessary, large-scale or local, crustal extension required for granite emplacement can be obtained. N° de réf. du vendeur 9780792344605
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