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Fluid Movements - Element Transport and the Composition of the Deep Crust
David Bridgwater
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Description for Fluid Movements - Element Transport and the Composition of the Deep Crust
Paperback. Proceedings of the NATO Advanced Research Workshop, Lindas, Norway, May 18-24, 1987 Series: NATO Science Series C. Num Pages: 440 pages, biography. BIC Classification: PHVG; PNV; RBG. Category: (P) Professional & Vocational. Dimension: 234 x 156 x 22. Weight in Grams: 670.
Many geologists have an equivocal attitude to fluid movements within the crust and the associated changes in the chemical and physical properties of crustal rocks. The controversies earlier this centuary between the "soaks" and the "pontiffs" memorably summarised by H. H. Read (1957) in The Granite Controversy have largely been resolved. Few would now advocate the formation of large granitic bodies by in situ transformation of pre-existing crust as the result of the passage of ichors without the formation of a granitic melt. To many geochemists fluid transport and metasomatism have become slightly suspect processes which at the most locally ... Read more
Many geologists have an equivocal attitude to fluid movements within the crust and the associated changes in the chemical and physical properties of crustal rocks. The controversies earlier this centuary between the "soaks" and the "pontiffs" memorably summarised by H. H. Read (1957) in The Granite Controversy have largely been resolved. Few would now advocate the formation of large granitic bodies by in situ transformation of pre-existing crust as the result of the passage of ichors without the formation of a granitic melt. To many geochemists fluid transport and metasomatism have become slightly suspect processes which at the most locally ... Read more
Product Details
Format
Paperback
Publication date
2011
Publisher
Springer Netherlands
Number of pages
440
Condition
New
Series
NATO Science Series C
Number of Pages
436
Place of Publication
Dordrecht, Netherlands
ISBN
9789401069359
SKU
V9789401069359
Shipping Time
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Ref
99-15
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