H2o and ultrahigh-pressure subsolidus phase relations for mafic and ultramafic systems

International Geology Review

Volumn 41, Issue 10, 1999, Pages 886-894

  Ernst, W G ^a  

^a STANFORD UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

PHASE EQUILIBRIUM; SUBDUCTION; ULTRAHIGH PRESSURE METAMORPHISM; WATER;

EID: 0033375447     PISSN: 00206814     EISSN: 19382839     Source Type: Journal    
DOI: 10.1080/00206819909465176     Document Type: Article

References (69)

1. Apted, M. J., and Liou, J. G., 1983. Phase relations among greenschist, epidote-amphibolite, and amphibolite in a basaltic system. Amer. Jour. Sci., 283A:328–353.
2. Austrheim, H., 1990. The granulite-eclogite facies transition:A comparison of experimental work and a natural occurrence in the Bergen Arcs, western Norway. Lithos, 25:163–169.
3. Austrheim, H., 1998. “ The influence of fluid and deformation on metamorphism of the deep crust and consequences for geodynamics of collision zones ”. In When continents collide:Geodynamics and geochemistry of ultrahigh-pressure rocks, Edited by:Hacker, B. R., and Liou, J. G., 297–323. Dordrecht:Kluwer Acad. Publ.
4. Bebout, G. E., 1996. Volatile transfer and recycling at convergent margins:Mass-balance and insights from high-P/T metamorphic rocks. Amer. Geophys. Union, Geophys. Monog., 96:179–193.
5. Bonattie, E., 1976. Serpentinite protrusions in the oceanic crust. Earth Planet. Sci. Lett., 32:107–113.
6. Brearley, A. J., 1987. An experimental and kinetic study of the breakdown of aluminous biotite at 800°C:Reaction microstructures and mineral chemistry. Bull. Mineral., 110:513–532.
7. 2O on the disequilibrium breakdown of muscovite + quartz. Jour. Petrol., 31:925–956.
8. Carmen, J. H., and Gilbert, M. C., 1983. Experimental studies of glaucophane stability. Amer. Jour. Sci., 283A:414–437.
9. Christensen, N. I., and Salisbury, M. H., 1975. Structure and constitution of the lower oceanic crust. Rev. Geophys. Space Phys., 13:57–86.
10. Coleman, R. G., 1971. Petrologic and geophysical nature of serpentinites. Geol. Soc. Amer. Bull., 82:897–918.
11. Drummond, M. S., and Defant, M. J., 1990. A model for trondhjemite-tonalite-dacite genesis and crustal growth via slab melting:Archean to modern comparisons. Jour. Geophys. Res., 95:21,503–21,521.
12. Ernst, W. G., 1990. Thermobarometric and fluid-expulsion history of subduction zones. Jour. Geophys. Res., 95:9047–9053.
13. Essene, E., Henson, B. J., and Green, D. H., 1970. Experimental study of amphibolite and eclogite stability. Phys. Earth Planet. Inter., 3:378–384.
14. Evans, B. W., Johannes, W., Oterdoom, H., and Trommsdorff, V., 1976. Stability of chrysotile and antigorite in the serpentinite multisystem. Schweiz. Mineral. Petrog. Mitteil., 56:79–93.
15. Frey, M., ed. 1987. Low temperature metamorphism, 351Glasgow:Blackie Publ.
16. Gardien, V., Thompson, A. B., Grujic, D., and Ulmer, P., 1995. Experimental melting of biotite + plagioclase + quartz ± muscovite assemblages and implications for crustal melting. Jour. Geophys. Res., 100:15,581–15,591.
17. Gilbert, M. C., Helz, R. T., Popp, R. K., and Spear, F. S., 1982. “ Experimental studies of amphibole stability ”. In Amphiboles:Petrology and experimental phase relations, Edited by:Veblen, D. R., and Ribbe, P. H., Vol. 9B, 229–353. Mineral. Soc. Amer., Rev. Mineral.
18. Hacker, B. R., 1990. Amphibolite-facies to granulite-facies reactions in experimentally deformed unpowdered amphibolite. Amer. Mineral., 75:1349–1361.
19. Hacker, B. R., 1991. The role of deformation in the formation of metamorphic field gradients:Ridge subduction beneath the Oman ophiolite. Tectonics, 10:455–473.
20. 2O content of oceanic crust. Amer. Geophys. Union, Geophys. Monog., 96:171–178.
21. Hawkesworth, C. J., Gallagher, K., Hergt, J. M., and McDermott, F., 1993. Mantle and slab contributions in an arc magma. Ann. Rev. Earth Planet. Sci., 21:175–204.
22. 2O = 5 kb as a function of oxygen fugacity. Jour. Petrol., 14:249–302.
23. Helz, R. T., 1979. Alkali exchange between hornblende and melt:A temperature-sensitive reaction. Amer. Mineral., 64:953–965.
24. Hirajima, T., Wallis, S., Zhai, R., and Ye, K., 1993. Eclogitized metagranitoid from the Su-Lu ultrahigh-pressure (UHP) province, eastern China. Proc. Japan Acad., 69:249–254.
25. Johannes, W., 1975. Zur synthese und thermischen stability von antigorit. Fortschrit für Mineral., 53:36
26. 2O:A model diagenetic reaction. Amer. Mineral., 82:781–789.
27. 2O at high pressures. Contrib. Mineral. Petrol., 79:258–267.
28. Kushiro, I., 1990. Partial melting of mantle wedge and evolution of island arc crust. Jour. Geophys. Res., 95:15,929–15,939.
29. Le Breton, N., and Thompson, A. B., 1988. Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexis. Contrib. Mineral. Petrol., 99:226–237.
30. Liu, J., Bohlen, S. R., and Ernst, W. G., 1996. Stability of hydrous phases in subducting oceanic crust. Earth Planet. Sci. Lett., 143:161–171.
31. Liou, J. G., Kuniyoshi, S., and Ito, K., 1974. Experimental studies of the phase relations between greenschist and amphibolite in a basaltic system. Amer. Jour. Sci., 274:613–632.
32. Liou, J. G., and Zhang, R. Y., 1996. Occurrences of inter-granular coesite in ultrahigh-P rocks from the Sulu region, eastern China:Implications for lack of fluid during exhumation. Amer. Mineral., 81:1217–1221.
33. Liou, J. G., Zhang, R. Y., Ernst, W. G., Rumble, D., III and Maruyama, S., 1998. High pressure minerals from deeply subducted metamorphic rocks. Rev. Mineral., 37:33–96.
34. Luth, R. W., 1997. Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa. Amer. Mineral., 82:1198–1209.
35. Maresch, W. V., 1977. Experimental studies of glaucophane:An analysis of present knowledge. Tectonophys., 43:109–125.
36. Massone, 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.
37. 2O. Lithos, 41:229–250.
38. Moody, J. B., Meyer, D., and Jenkins, J. E., 1983. Experimental characterization of the greenschist/amphibolite boundary in mafic systems. Amer. Jour. Sci., 283:48–92.
39. Morris, P. A., 1995. Slab melting as an example of Quaternary volcanism and aseismicity in southwest Japan. Geology, 23:395–398.
40. Mosenfelder, J. L., and Bohlen, S. R., 1997. Kinetics of the coesite to quartz transformation. Earth Planet. Sci. Lett., 153:133–147.
41. Mysen, B. O., Ulmer, P., Konzett, J., and Schmidt, M. W., 1998. The upper mantle near convergent plate boundaries. Rev. Mineral., 37:97–138.
42. Nichols, G. T., Wyllie, P. J., and Stern, C. R., 1996. Experimental melting of pelagic sediment, constraints relevant to subduction. Amer. Geophys. Union, Geophys. Monog., 96:293–298.
43. 2O system. Amer. Mineral., 84:362–373.
44. Ono, S., 1998. Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions:Implications for water transport in subduction zones. Jour. Geophys. Res., 103:18,253–18,267.
45. 2), and Mg/Fe ratio on dehydration-melting of model metagraywackes. Jour. Petrol., 37:999–1024.
46. 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 rocks, Edited by:Hacker, B. R., and Liou, J. G., 27–55. Dordrecht:Kluwer Acad. Publ.
47. 2O:New experimental results and petrological implications. Amer. Mineral., 83:51–57.
48. Pawley, A. R., and Holloway, J. R., 1993. Water sources for subduction zone volcanism:New experimental constraints. Science, 260:664–667.
49. Peacock, S. M., 1990. Fluid processes in subduction zones. Science, 248:329–337.
50. Peacock, S. M., 1995. Ultrahigh-pressure metamorphic rocks and the thermal evolution of continent collision belts. The Island Arc, 4:376–383.
51. Poli, S., 1993. The amphibolite-eclogite transformation:An experimental study on basalt. Amer. Jour. Sci., 293:1061–1107.
52. Poli, S., and Schmidt, M. W., 1997. The high-pressure stability of hydrous phases in orogenic belts:An experimental approach on eclogite-forming processes. Techtonophys., 273:169–184.
53. Ridley, J., 1985. “ The effect of reaction enthalpy on the progress of a metamorphic reaction ”. In Metamorphic reactions:Kinetics, textures, and deformation, Edited by:Thompson, A. B., and Rubie, D. C., 80–97. New York:Springer-Verlag.
54. Rubie, D. C., 1986. The catalysis of mineral reactions by water and restrictions on the presence of aqueous fluid during metamorphism. Mineral. Mag., 50:399–415.
55. Rubie, D. C., 1990. “ Role of kinetics in the formation and pres ervation of eclogites ”. In Eclogite facies rocks, Edited by:Carswell, D. A., 111–140. New York:Chapman and Hall.
56. Rubie, D. C., and Brearley, A. J., 1987. Metastable melting during the breakdown of muscovite + quartz at 1 kbar. Bull. Mineral., 110:533–549.
57. Schmidt, M. W., and Poli, S., 1994. The stability of lawsonite and zoisite at high pressures:Experiments in CASH to 92 kbar and implications for the presence of hydrous phases in subducted lithosphere. Earth Planet. Sci. Lett., 124:105–118.
58. 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.
59. Schramke, J. A., Kerrick, D. M., and Lasaga, A. C., 1987. The reaction muscovite + quartz ↔ andalusite + K-feldspar + water:Part 1, growth kinetics and mechanism. Amer. Jour. Sci., 287:517–559.
60. Schreyer, W., Massone, 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:Physico-chemical principles, The Geochem. Soc. Spec. Publ. no. 1 Edited by:Mysen, B. O., 155–163.
61. Skjerlie, K. P., and Johnston, A. D., 1996. Vapor-absent melting from 10 to 20 kbar of crustal rocks that contain multiple hydrous phases:Implications for anatexis in the deep to very deep continental crust and active continental margins. Jour. Petrol., 37:661–691.
62. Spear, F. S., 1981. An experimental study of hornblende stability and compositional variability in amphibolite. Amer. Jour. Sci., 281:697–734.
63. Ulmer, P., and Trommsdorff, V., 1995. Serpentine stability to mantle depths and subduction-related magmatism. Science, 268:858–861.
64. Vielzeuf, D., and Holloway, J. R., 1988. Experimental determination of the fluid-absent melting relations in the pelitic system. Consequences for crustal differentiation. Contrib. Mineral. Petrol., 98:257–276.
65. Vielzeuf, D., and Montel, J. M., 1994. Partial melting of metagraywackes. 1. Fluid-absent experiments and phase relationships. Contrib. Mineral. Petrol., 117:375–393.
66. 2O. Amer. Jour. Sci., 283A:151–180.
67. 4 (NMASF):Some implications for glaucophane stability in natural and synthetic systems at high temperatures and pressures. Contrib. Mineral. Petrol., III:248–259.
68. 2O (MSH). Lithos, 41:213–227.
69. Zhang, R. Y., and Liou, J. G., 1997. Partial transformation of gabbro to coesite-bearing eclogite from Yangkou, the Sulu terrene, eastern China. Jour. Metamor. Geol., 15:183–202.