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Understanding granites : integrating new and classical techniques

Author: Antonio Castro; Carlos Fernández Rodríguez; Jean Louis Vigneresse
Publisher: London : Geological Society, 1999.
Series: Geological Society special publication, no. 168.
Edition/Format:   eBook : Document : EnglishView all editions and formats
Summary:
Granite magmatism represents a major contribution to crustal growth and recycling and, consequently, is one of the most important mechanisms to have contributed to the geochemical differentiation of the Earth's crust since Archaean time. Granites are also often associated with ore bodies, and their study therefore has direct commercial relevance. The modern view of the granite problems requires the application of  Read more...
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Additional Physical Format: Print version:
Understanding granites.
London : Geological Society, 1999
(OCoLC)43186353
Material Type: Document, Internet resource
Document Type: Internet Resource, Computer File
All Authors / Contributors: Antonio Castro; Carlos Fernández Rodríguez; Jean Louis Vigneresse
ISBN: 1423784421 9781423784425
OCLC Number: 190784884
Description: 1 online resource (278 pages) : illustrations.
Contents: Understanding granites: integrating new and classical techniques / A. Castro, C. Fernández, J.L. Vigneresse --
Some time-space relationships for crustal melting and granitic intrusion at various depths / A.B. Thompson --
Granitic melt viscosities / D.B. Dingwell --
Geophysical imaging of the shape of granitic intrusions at depth: a review / L. Améglio, J.L. Vigneresse --
What do experiments tell us about the relative contribution of crust and mantle to the origin of granitic magmas? / A.E. Patiño Douce --
Geometry of granite emplacement in the upper crust: contributions of analogue modelling / T. Román-Berdiel --
A multidisciplinary approach combining geochemical, gravity and structural data: implications for pluton emplacement and zonation / L. Hecht, J.L. Vigneresse --
The Coastal Batholith and other aspects of Andean magmatism in Peru / J.E. Cobbing --
Contrasts in morphogenesis and tectonic setting during contemporaneous emplacement of S- and I-type granitoids in the Eastern Lachlan fold belt, southeastern Australia / R. Trzebski, P. Lennox, D. Palmer --
Structure and geophysics of the Gasborn granite, central Sweden: an example of fracture-fed asymmetric pluton emplacement / A.R. Cruden, H. Sjöström, S. Aaro --
Emplacement of the Joshua Flat-Beer Creek Pluton (White Inyo Mountains, California): a story of multiple material transfer processes / C. Dietl --
Petrology, magnetic fabric and emplacement in the strike-slip regime of a zoned peraluminous granite: the Campanario-La Haba pluton, Spain / A. Alonso Olazabal, M. Carracedo, A. Aranguren --
Brittle behaviour of granitic magma: the example of Puente del Congosto, Iberian Massif, Spain / C. Fernández, A. Castro --
Origin of megacrysts in granitoids by textural coarsening: a crystal size distribution (CSD) study of microline in the Cathedral Peak granodiorite, Sierra Nevada, California / M.D. Higgins --
Movement of melt during synchronous regional deformation and granulite-facies anatexis: an example from the Wuluma Hills, Central Australia / E.W. Sawyer, C. Dombrowski, W.J. Collins --
Partial melting and P-Tt evolution of LP/HT metamorphic terranes: an example from the Svecofennian K-feldspar-poor leucosome migmatite belt, southern Finland / H. Mouri, K. Korsman --
Magmatic hybridization related with feeding zones: the synkinematic Guitiriz granitoid, northwest Iberian Massif, Spain / M. Menéndez, L.A. Ortega.
Series Title: Geological Society special publication, no. 168.
Responsibility: edited by Antonio Castro, Carlos Fernández, and Jean Louis Vigneresse.

Abstract:

Granite magmatism represents a major contribution to crustal growth and recycling and, consequently, is one of the most important mechanisms to have contributed to the geochemical differentiation of the Earth's crust since Archaean time. Granites are also often associated with ore bodies, and their study therefore has direct commercial relevance. The modern view of the granite problems requires the application of many different theoretical, experimental and empirical resources provided by geophysics, geochemistry, experimental petrology, structural geology, scale modelling and field geology. Because of the complexity of the granite problem, it is necessary to integrate a variety of techniques and corroborate the findings with field observations. This is the philosophy of this book.

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