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Crustal anatexis

The behavior of apatite during crustal anatexis equilibrium and kinetic... [Pg.604]

Wickham SM, Taylor HP (1987) Stable isotope constraints on the origin and depth of penetration of hydrothermal fluids associated with Hercynian regional metamorphism and crustal anatexis in the Pyrenees. Contrib Mineral Petrol 95 255-268... [Pg.118]

Frezzotti ML, Zanon V, Peccerillo A, Nikogossian I (2004b) Silica-rich melts in quartz xenoliths from Vulcano island and their bearing on processes of crustal anatexis and crust-magma interaction beneath the Aeolian Arc, southern Italy. J Petrol 45 3-26... [Pg.340]

Wickham S. M. and Taylor H. P., Jr. (1990) Hydrothermal systems associated with regional metamorphism and crustal anatexis examples from the Pyrenees, France. In The Role of Fluids in Crustal Processes (Geophysical Study Committee, Commission on Geosciences, Environment and Resources, National Research Council). National Academy Press, Washington, DC, pp. 96-112. [Pg.1491]

DeYoreo J. J., Lux D. R., and Guidotti C. V. (1989) The role of crustal anatexis and magma migration in the in the thermal evolution of regions of thickened crust. In Evolution of Metamorphic Belts, Special Publications 43 (eds. J. S. Daly, R. A. Cliff, and B. W. D. Yardley). Geological Society of London, London, England, pp. 187 -202. [Pg.1549]

Flood R. H. and Vernon R. H. (1978) The Cooma Granodiorite, Australia an example of in situ crustal anatexis Geology 6, 81-84. [Pg.1667]

Kemp A. I. S. and Ch-ay C. M. (1999) Geological context of crustal anatexis and granitic magmatism in the northeastern Glenelg River Complex, western Victoria. Austral J. Earth Sci. 46, 406-420. [Pg.1668]

McDermott F., Harris N. B. W., and Hawkesworth C. J. (1996) Geochemical constraints on crustal anatexis a case study from the Pan-African Damara granitoids of Namibia. Contrib. Mineral. Petrol. 123, 406-423. [Pg.1669]

Harrison, T. M., and E. B. Watson, The behavior of apatite during crustal anatexis equi-... [Pg.28]

Anatexis of subducted oceanic lithosphere generates relatively uraniferous magmas. Continental andesites range from 0.5 to 1.0 ppm uranium, whereas island-arc andesites range from 0.2 to 0.4 ppm. Enrichment in continental andesites is probably due to continental crustal contamination. Fractionation of andesitic magmas can separate uranium, alkaline-earth... [Pg.90]

The origin of pegmatitic alkalic granites is somewhat in question. Some writers believe that they are derived from the mantle, but others contended that they form through anatexis of lower crustal material. Murphy et al. suggested... [Pg.122]

See other pages where Crustal anatexis is mentioned: [Pg.4]    [Pg.39]    [Pg.47]    [Pg.189]    [Pg.1632]    [Pg.1636]    [Pg.1649]    [Pg.1659]    [Pg.40]    [Pg.168]    [Pg.4]    [Pg.39]    [Pg.47]    [Pg.189]    [Pg.1632]    [Pg.1636]    [Pg.1649]    [Pg.1659]    [Pg.40]    [Pg.168]    [Pg.116]    [Pg.1618]    [Pg.1628]    [Pg.1637]    [Pg.1640]    [Pg.1658]    [Pg.37]    [Pg.328]    [Pg.523]    [Pg.106]   
See also in sourсe #XX -- [ Pg.38 , Pg.270 , Pg.295 ]



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Anatexis

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