Experimental aspects of uhp metamorphism: Granitic systems

International Geology Review

Volumn 41, Issue 8, 1999, Pages 701-710

  Schreyer, Werner ^a  

^a RUHR UNIVERSITY BOCHUM   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

EXPERIMENTAL DESIGN; GRANITE; PETROLOGY; ULTRAHIGH PRESSURE METAMORPHISM;

EID: 0033396522     PISSN: 00206814     EISSN: 19382839     Source Type: Journal    
DOI: 10.1080/00206819909465165     Document Type: Article

References (28)

1. Adam, J., Green, T. H., Sie, S. H., and Ryan, C. G., 1997. Trace element partitioning between aqueous fluids, silicate melts, and minerals. Eur. Jour. Mineral., 9:569–584.
2. Boettcher, A. L., and Wyllie, P. J., 1968. Melting of granite with excess water to 30 kilobars pressure. Jour. Geol., 76:235–244.
3. Burchard, M., and Schreyer, W., 1995a. Melting experiments on the granitic country rock of the Dora Maira pyrope quartzites. Bochum. Geol. Geotech. Arb., 44:23–27.
4. Burchard, M., and Schreyer, W., 1995b. Coexisting phases in the granitic country rock of the Dora Maira pyrope-quartzites reacted at 30 kbar, 600–900°C with variable water quantities [abs.]. Berichte der Deutschen Mineralogischen Gesellschaft, Beih. z. Eur. Jour. Mineral., 7:41
5. Bureau, H., and Keppler, H., 1999. Complete miscibility between silicate melts and hydrous fluids in the upper mantle:Experimental evidence and geochemical implications. Earth Planet. Sci. Lett., 165:187–196.
6. Chopin, C., Henry, C., and Michard, A., 1991. Geology and petrology of the coesite-bearing terrain, Dora Maira massif, Western Alps. Eur. Jour. Mineral., 3:263–291.
7. 2O recycling during continental collision:Phase-equilibria and kinetic constraints ”. In When continents collide:Geodynamics and geochemistry of ultra-high-pressure rocks, Edited by:Hacker, B. R., and Liou, J. G., 275–295. Dordrecht:Kluwer Acad., Publ.
8. Goldsmith, J. R., and Jenkins, D. M., 1985. The hydrothermal melting of low and high albite. Amer. Mineral, 70:924–933.
9. 2 to 35 kilobars, dry and with excess water. Jour. Geol., 83:737–748.
10. 2O to 35 kbar:Muscovite granite from Harney Peak, South Dakota. Jour. Geophys. Res., 86:10,515–10,529.
11. 2O. Amer. Jour. Sci., 260:501–521.
12. 2O (KMASH). Lithos, 28:421–434.
13. Massonne, H.-J., 1995. “ Experimental and petrogenetic study of UHPM ”. In Ultrahigh pressure metamorphism, Edited by:Coleman, R. G., and Wang, X., 33–95. New York:Cambridge University Press.
14. 2 component on the low quartz-coesite transition. Jour. Geophys. Res., 85:6983–6990.
15. 2O phase relationships and critical behavior at high pressures. Contrib. Mineral. Petrol., 112:490–500.
16. Patiño Douce, A. E., and McCarthy, T. C., 1998. “ Melting of crustal rocks during continental collision and subduction ”. In When continents collide:Geodynamics and geochemistry of ultrahigh-pressure metamorphism, Edited by:Hacker, B. R., and Liou, J. G., 27–55. Dordrecht:Kluwer Acad. Publ.
17. Schertl, H.-P., Schreyer, W., and Chopin, C., 1991. The pyropecoesite rocks and their country rocks at Parigi, Dora-Maira Massif, Western Alps:Detailed petrography, mineral chemistry and P-T path. Contrib. Mineral. Petrol., 108:1–21.
18. Schmidt, M. W., 1996. Experimental constraints on recycling of potassium from subducted oceanic crust. Science, 272:1927–1930.
19. Schmidt, M. W., and Poli, S., 1998. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet. Sci. Lett., 163:361–379.
20. Schreyer, W., Massonne, H.-J., and Chopin, C., 1987. “ Continental crust subducted to depths near 100 km:Implications for magma and fluid genesis in collision zones ”. In Magmatic processes:Physicochemical principles, Edited by:Mysen, B., 155–163. The Geochem. Soc., Spec. Publ. 1.
21. 2O system. Nature, 385:710–712.
22. Stern, C. R., and Wyllie, P. J., 1973. Water-saturated and undersaturated melting relations of a granite to 35 kilobars. Earth Planet. Sci. Lett., 18:163–167.
23. 2O to 35 kilobars:The Dinkey Lakes biotite-granite from the Sierra Nevada Batholith. Jour. Geophys. Res., 86:10,412–10,422.
24. Stockhert, B., and Renner, J., 1998. “ Rheology of crustal rocks at ultrahigh pressure ”. In When continents collide:Geodynamics and geochemistry of ultrahigh-pressure rocks, Edited by:Hacker, B. R., and Liou, J. G., 57–95. Dordrecht:Kluwer Acad. Publ.
25. Tilton, G. R., Schreyer, W., and Schertl, H.-P., 1991. Pb-Sr-Nd isotopic behavior of deeply subducted crustal rocks from the Dora-Maira Massif, Western Alps:What is the age of the ultrahigh-pressure metamorphism?. Contrib. Mineral. Petrol., 108:22–33.
26. 2. Contrib. Mineral. Petrol., 121:61–73.
27. Wilson, M., 1989. Igneous petrogenesis, London:Harper Collins Acad. 466 p.
28. Wyllie, P. J., Wolf, M. B., and van der Laan, S. R., 1996. “ Conditions for formation of tonalities and trondhjemites:Magmatic sources and products ”. In Tectonic evolution of greenstone belts, Edited by:de Wit, M. J., and Ashwahl, L. D., 258–267. Oxford, U.K.:Oxford University Press.