Fluid-rock interactions during high-pressure and ultrahigh-pressure metamorphism

International Geology Review

Volumn 42, Issue 4, 2000, Pages 312-327

  Philippot, P ^a   Iii, D Rumble ^b  

^a UNIVERSITÉ PARIS DESCARTES   (France)

^b GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CONTINENTAL COLLISION; CONTINENTAL CRUST; HIGH PRESSURE; METAMORPHISM; OCEANIC CRUST; SLAB; SUBDUCTION; ULTRAHIGH PRESSURE METAMORPHISM; WATER-ROCK INTERACTION;

EID: 0034078375     PISSN: 00206814     EISSN: 19382839     Source Type: Journal    
DOI: 10.1080/00206810009465085     Document Type: Article

References (98)

1. Agard, P., 1999. Evolution métamorphique et structurale des métapélites océaniques dans l'orogène alpin:l'exemple des schistes lustrés des Alpes occidentales, 279Paris:Université Jussieu. Unpubl. Ph.D. thesis
2. Agrinier, P., Hekinian, R., Bideau, D., and Javoy, M., 1995. O and H stable isotope compositions of oceanic crust and upper mantle rocks in the Hess Deep near the Galapagos Triple Junction. Earth Planet. Sci. Lett., 136:183–196.
3. Agrinier, P., Laverne, C., and Tartarotti, P., 1995. “ Stable isotope ratios (oxygen, hydrogen) and petrology of hydrothermally altered dolerites at the bottom of the sheeted dike complex of Hole 504B ”. In Proc. Ocean Drilling Program, Science Results Edited by:Erzinger, J., Becker, K., Dick, H. J. B., and Stokking, L. B., 99–106. College Station, TX
4. Anderson, A. T., 1967. The dimensions of oxygen isotopic equilibrium attainment during prograde metamorphism. Jour. Geol., 75:323–332.
5. Austrheim, H., 1987. Eclogitization of lower crustal granulites by fluid migration through shear zones. Earth Planet. Sci. Lett., 81:221–232.
6. Baker, J., Matthews, A., Mattey, D., Rowley, D. B., and Xue, F., 1997. Fluid-rock interaction during ultra-high pressure metamorphism, Dabie Shan, China. Geochim. et Cosmochim. Acta, 61:1685–1696.
7. Barnicoat, A. C., and Cartwright, I., 1997. Focused fluid flow during subduction:Oxygen isotope data from high pressure ophiolites of the western Alps. Earth Planet. Sci. Lett., 132:53–61.
8. 18O terranes tracking Mesozoic polar climates in the South Pacific. Geochim. et Cosmochim. Acta, 61:569–576.
9. 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.
10. Chopin, C., 1984. Coesite and pure pyrope in high grade blueschists of the Western Alps:A first record and some consequences. Contrib. Mineral. Petrol., 86:107–118.
11. Criss, R. E., and Taylor, H. P., 1986. “ Meteoric-hydrothermal systems ”. In Stable isotopes in high temperature geological Processes, Edited by:Valley, J. W., Taylor, H. P., and O'Neil, J. R., Vol. 16, 373–424. Washington, DC:Mineral. Soc. Amer.
12. Dal Piaz, G., 1974. Le métamorphisme alpin de haute pression et basse température dans l'évolution structurale du bassin ophiolitique alpino-apenninique. Schweiz. Mineral. Petrog. Mitteil., 54:399–424.
13. Dal Piaz, G. V., Venturelli, G., and Scolari, A., 1979. Calc-alkaline to ultrapotassic postcollisional volcanic activity in the internal northwestern Alps. Mem. Sci. Geol. Padova, 32:16
14. Desmons, J., and O'Neil, J. R., 1978. Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia Zone (Western Alps, Italy). Contrib. Mineral. Petrol., 67:79–85.
15. Domanik, K. J., and Holloway, J. R., 1998. “ Experimental determination of the stability and phase relations of phengitic muscovite in a calcareous metapelite from the Dabie Mountains, China ”. In Int. Workshop on UHP Metamorphism and Exhumation, Edited by:Liou, J. G., and Ernst, W. G., A206–A207. Stanford:Stanford Univ.
16. Eiler, J. M., Baumgartner, L. P., and Valley, J. W., 1992. Intercrystalline stable isotope diffusion:A fast grain boundary model. Contrib. Mineral. Petrol., 112:543–557.
17. Ernst, W. G., 1999. Metamorphism, partial preservation, and exhumation of ultrahigh-pressure belts. The Island Arc, 8:125–153.
18. Farquhar, J., Chacko, T., and Ellis, D. J., 1996. Preservation of oxygen isotope compositions in granulites from Northwestern Canada and Enderby Land, Antarctica:Implications for high-temperature isotopic thermometry. Contrib. Mineral. Petrol., 125:213–224.
19. Ferry, J. M., and Gerdes, M. L., 1998. Chemically reactive fluid flow during metamorphism. Ann. Rev. Earth Planet. Sci., 26:255–287.
20. Früh-Green, G. L., 1994. Interdependence of deformation, fluid infiltration, and reaction progress recorded in eclogitic metagranitoids (Sesia Zone, western Alps). Jour. Metamor. Geol., 12:327–343.
21. Früh-Green, G. L., Plas, A., and Lecuyer, C., 1996. “ Petrologic and stable isotope constraints on hydrothermal alteration and serpentinization of the EPR shallow mantle at Hess Deep (site 895) ”. In Proc. of the Ocean Drilling Program, Scientific Results Edited by:Mevel, C., Gillis, K. M., Allan, J. F., and Meyer, P. S., 255–287. College Station, TX
22. Fu, B., Zheng, Y. F., Wang, Z., Xiao, Y., Gong, B., and Li, S., 1999. Oxygen and hydrogen isotope geochemistry of gneisses associated with ultrahigh pressure eclogites at Shuanghe in the Dabie Mountains. Contrib. Mineral. Petrol., 134:52–66.
23. Ganor, J., Matthews, A., Schliestedt, M., and Garfunkel, Z., 1996. Oxygen isotope heterogeneities of metamorphic rocks:An original tectonostratigraphic signature, or an imprint of exotic fluids? A case study of Sifnos and Tinos islands (Greece). Eur. Jour. Mineral., 8:719–732.
24. Getty, S. R., and Selverstone, J., 1994. Stable isotope and trace element evidence for restricted fluid migration in 2 GPa eclogites. Jour. Metamor. Geol., 12:747–760.
25. Giletti, B. J., 1986. Diffusion effects on oxygen isotope temperatures of slowly cooled igneous and metamorphic rocks. Earth Planet. Sci. Lett., 77:218–228.
26. 2 in natural wollastonite-hosted fluid inclusions. Contrib. Mineral. Petrol., 122:51–61.
27. Jahn, B. M., 1998. “ Geochemical and isotopic characteristics of UHP eclogites and ultramafic rocks of the Dabie orogen:Implications for continental subduction and collisional tectonics ”. In When continents collide:Geodynamics and geochemistry of ultrahigh-pressure rocks, Edited by:Hacker, B. R., and Liou, J. G., 203–239. Dordrecht:Kluwer Acad. Publ.
28. Jamtveit, B., Bucher-Nurminen, K., and Austrheim, H., 1990. Fluid controlled eclogitization of granulites in deep crustal shear zones, Bergen arcs, Western Norway. Contrib. Mineral. Petrol., 104:184–193.
29. Jenkin, G. R. T., Farrow, C. M., Fallick, A. E., and Higgins, D., 1994. Oxygen isotope exchange and closure temperatures in cooling rocks. Jour. Metamor. Geol., 12:221–235.
30. 2 mixtures at elevated pressures and temperatures. Amer. Jour. Sci., 281:735–767.
31. Kirby, S. H., Engdahl, E. R., and Denlinger, R., 1996. “ Intermediate-depth intraslab earthquakes and arc volcanism as physical expressions of crustal and uppermost mantle metamorphism in subducting slabs ”. In Subduction top to bottom, Edited by:Bebout, G. E., Scholl, D. W., Kirby, S. H., and Platt, J. P., 195–214. Washington, DC:Amer. Geophys. Union.
32. Luckscheiter, B., and Morteani, G., 1980. Microthermometrical and chemical studies of fluid inclusions from Alpine veins from the penninic rocks of the central and western Tauern Window, Austria, Italy. Lithos, 13:61–77.
33. 2O in the lower crust and upper mantle. Geochim. et Cosmochim. Acta, 58:4831–4839.
34. 2O-HCl. Schweiz. Mineral. Petrog. Mitteil., 78:225–242.
35. 2O at 700 Deg C., 1 and 1.5 GPA:Evidence of high Al mobility in deep metasomatic environments. Geol. Soc. Amer. Abs. Prog., 1999:A354
36. Manning, C. E., and Ingebritsen, S. E., 1999. Permeability of the continental crust:Implications of geothermal data and metamorphic systems. Rev. Geophys. Space Phys., 37:127–150.
37. Marion, E., 1992. Intéractions croûte océanique profonde-eau de mer dans les gabbros de la zone M.A.R.K., Vol. 6, 159Paris:Université Paris. Unpubl. Ph.D. thesis
38. Matthews, A., Liata, A., Mposkos, E., and Skarpelis, N., 1996. Oxygen isotope geochemistry of the Rhodope polymetamorphic terrain in northern Greece:Evidence for preservation of pre-metamorphic isotopic compositions. Eur. Jour. Mineral., 8:1139–1152.
39. 2O (KMASH). Lithos, 28:421–434.
40. Messiga, B., 1987. Alpine metamorphic evolution of Ligurian Alps (North-West Italy):Chemography and petrological constraints inferred from metamorphic climax assemblages. Contrib. Mineral. Petrol., 95:269–277.
41. Messiga, B., Kienast, J. R., Rebay, G., Riccardi, M. P., and Tribuzio, R., 1999. Cr-rich magnesochloritoid eclogites from the Monviso ophiolites (western Alps, Italy). Jour. Metamor. Geol., 17:287–299.
42. Messiga, B., and Scambelluri, M., 1988. Comparison between two types of coronitic eclogites from the western Alps:Implications for a pre-eclogitic evolution. Schweiz. Mineral. Petrog. Mitteil., 68:225–235.
43. Messiga, B., Scambelluri, M., and Piccardo, G. B., 1995. Chloritoid-bearing assemblages in mafic systems and the eclogitic hydration of Alpine Mg-Al metagabbros (Erro-Tobbio unit, Ligurian Western Alps). Eur. Jour. Mineral., 7:1149–1167.
44. Mével, C., Caby, R., and Kienast, J. R., 1978. Amphibolite facies conditions in the oceanic crust:Example of amphibolitized flaser gabbros and amphibolites from the Chenaillet ophiolite massif (Hautes Alpes, France). Earth Planet. Sci. Lett., 39:98–108.
45. Mibe, K., Fujii, T., and Yasuda, A., 1999. Control of the location of the volcanic front in island arcs by aqueous fluid connectivity in the mantle wedge. Nature, 401:259–262.
46. Muehlenbachs, K., 1986. “ Alteration of the oceanic crust and the 18O history of seawater ”. In Stable isotopes in high temperature geological processes, Edited by:Valley, J. W., Taylor, H. P. J., and O'Neil, J. R., Vol. 16, 425–444. Mineral. Soc. Amer., Rev. Mineral.
47. Nadeau, S., Philippot, P., and Pineau, F., 1993. Fluid inclusion and mineral isotopic compositions (H-C-O) in eclogite rocks as tracers of local fluid migration during high pressure metamorphism. Earth Planet. Sci. Lett., 114:431–448.
48. Peacock, S. M., and Wang, K., 1999. Seismic consequences of warm versus cool subduction metamorphism:Examples from southwest and northeast Japan. Science, 286:937–939.
49. Philippot, P., 1987. Crack-seal vein geometry in eclogitic rocks. Geodin. Acta, 1:171–181.
50. Philippot, P., 1993. Fluid-melt-rock interaction in mafic eclo gites and coesite-bearing metasediments:Constraints on volatile recycling during subduction. Chem. Geol., 108:93–112.
51. Philippot, P., 1996. The composition of high-pressure fluids from the Alps:Natural observations vs. experimental constraints. Earth Sci. Frontiers, 3:39–52.
52. Philippot, P., Agrinier, P., and Scambelluri, M., 1998. Chlorine cycling during subduction of altered oceanic crust. Earth Planet. Sci. Lett., 161:33–44.
53. Philippot, P., Chevallier, P., Chopin, C., and Dubessy, J., 1995. Fluid composition and evolution in coesite bearing rocks (Dora Maira massif, western Alps):Implications for element recycling during subduction. Contrib. Mineral. Petrol., 121:29–44.
54. Philippot, P., and Selverstone, J., 1991. Trace-element brines in eclogitic veins:Implications for fluid composition and transport during subduction. Contrib. Mineral. Petrol., 106:417–430.
55. Pognante, U., 1981. Magmatic and metamorphic evolution of two Fe-Ti gabbroic series from the Piemonte ophiolite nappe in the Susa valley area, Italian Western Alps. Mem. Sci. Geol. Padova, 35:21–34.
56. Pognante, U., 1989. Early alpine eclogitization in talc/chloritoid-bearing Mg-metagabbros and in jadeite-Fe omphacite-bearing metatrondjemites from the ophiolites of the western Alps. Rend. Soc. Ital. Mineral. Petrol., 43:687–704.
57. 16O:comparaisons thermométriques et barométriques sur quelques éclogites et micaschists de la zone Sesia-Lanzo (Alpes italiennes). Bull. Mineral., 108:699–711.
58. Rumble, D., 1978. Mineralogy, petrology, and oxygen isotope geochemistry of the Clough Formation, Black Mountain, western New Hampshire, USA. Jour. Petrol., 19:317–340.
59. Rumble, D., 1998. “ Stable isotope geochemistry of ultra-high-pressure rocks ”. In When continents collide:Geodynamics and geochemistry of ultrahigh-pressure rocks, Edited by:Hacker, B. R., and Liou, J. G., 241–259. Dordrecht:Kluwer Acad. Publ.
60. Rumble, D., Ferry, J. M., Hoering, T. C., and Boucot, A. J., 1982. Fluid flow during metamorphism at the Beaver Brook fossil locality, New Hampshire. Amer. Jour. Sci., 282:886–919.
61. Rumble, D., and Spear, F. S., 1983. Oxygen-isotope equilibration and permeability enhancement during regional metamorphism. Jour. Geol. Soc. Lond., 140:619–628.
62. Rumble, D., Wang, Q. C., and Zhang, R. Y., Stable isotope geochemistry of marbles from UHP terrains in Dabie-shan and Sulu, China. Lithos
63. Rumble, D., and Yui, T. F., 1998. The Qinglongshan oxygen and hydrogen isotope anomaly near Donghai in Jiangsu province, China. Geochim. et Cosmochim. Acta, 62:3307–3321.
64. Ryabchikov, I. D., 1993. Fluid transport of ore metals in ultramafic mantle rocks. Proc. Eighth Quadrennial IAGOD Symp., 8:425–433.
65. Ryabchikov, I. D., and Boettcher, A. L., 1980. Experimental evidence at high pressure for potassic metasomatism in the mantle of the Earth. Amer. Mineral., 65:915–919.
66. Scambelluri, M., Muentener, O., Hermann, J., Piccardo, G. B., and Trommsdorff, V., 1995. Subduction of water into the mantle:History of an Alpine peridotite. Geology, 23:459–462.
67. Scambelluri, M., Pennacchioni, G., and Philippot, P., 1998. Salt rich aqueous fluids formed during eclogitisation of metabasites in the alpine continental crust (Austroalpine Mt. Emilius unit, Italian Western Alps). Lithos, 43:151–167.
68. Scambelluri, M., and Philippot, P., 2000. “ Deep cycling of fluids in subduction zones ”. In Fluid inclusion studies at the turn of the century, Eur. Mineral. Union.
69. Scambelluri, M., Piccardo, G., Philippot, P., Robbiano, A., and Negretti, L., 1997. High-salinity brines from recycled seawater in deeply subducted serpentinite. Earth Planet. Sci. Lett., 148:485–499.
70. 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.
71. Schreyer, W., 1988. Experimental studies on metamorphism of crustal rocks under mantle pressure. Mineral. Mag., 364:1–36.
72. 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:Physio-chemical principles, Edited by:Mysen, B. O., Vol. 1, 155–163. Univ. Park, PA:Geochem. Soc. Spec. Publ.
73. Selverstone, J., Franz, G., Thomas, S., and Getty, S. R., 1992. Fluid variability in 2 GPa eclogites as an indicator of fluid behaviour during subduction. Contrib. Mineral. Petrol., 112:341–357.
74. Sharp, Z. D., Essene, E. J., and Hunziker, J. C., 1993. Stable isotope geochemistry and phase equilibria of coe-site-bearing whiteschists, Dora Maira massif, western Alps. Contrib. Mineral. Petrol., 114:1–12.
75. 2O system. Nature, 385:710–712.
76. Sheppard, S. M. F., and Taylor, H. P., Jr. 1974. Hydrogen and oxygen isotope evidence for the origin of water in the Boulder batholith and the Butte ore deposits. Econ. Geol., 69:926–946.
77. Smith, D. C., 1984. Coesite in clinopyroxene in the Caledonides and its implications for geodynamics. Nature, 310:641–644.
78. Sobolev, N. V., and Shatsky, V. S., 1990. Diamond inclusions in garnets from metamorphic rocks. Nature, 343:742–746.
79. Svensen, H., Jamtveit, B., Yardley, B., Engvik, A. K., Austrheim, H., and Broman, C., 1999. Lead and bromine enrichment in eclogite-facies fluids:Extreme fractionation during lower-crustal hydration. Geology, 27:467–470.
80. Tatsumi, Y., 1989. Migration of fluid phases and genesis of basalt magmas in subduction zones. Jour. Geophys. Res., 94:4697–4707.
81. Thomas, S., 1991. Zur Kluftbildung in Gesteinen der Eklogitzone (Hohe Tauern, Osterreich), Technisches Universität Berlin. Unpubl. Ph.D. thesis
82. Ulmer, P., and Trommsdorff, V., 1995. Serpentinite stability to mantle depths and subduction-related magmatism. Science, 268:858–861.
83. Vallis, F., 1997. Stuglio degli isotopi stabili (H-O) nelle rocce ultrafemiche di ambiente eclogitico dell'unitá Erro-Tobbio (Alpi Occidentali):Implicazioni sul rilascio di fluidi durante la subduzione, 204Universitá di Genova. Unpubl. Ph.D. thesis
84. Vallis, F., Frueh-Green, G. L., Scambelluri, M., and Piccardo, G. B., 1997. Eclogitization of the Erro-Tobbio serpentinized peridotite:A stable isotope study, Fifth Int. Eclogite Conf. Vol. 9, 39Ascon, Switzerland:Terra Nova Abs. Supplement.
85. Vallis, F., and Scambelluri, M., 1996. Redistribution of high-pressure fluids during retrograde metamorphism of eclogite facies rocks (Voltri Massif, Italian Western Alps). Lithos, 39:81–92.
86. Valley, J. W., 1986. “ Stable isotope geochemistry of metamorphic rocks ”. In Stable isotopes in high temperature geological processes, Edited by:Valley, J. W., Taylor, H. P., Jr. and O'Neil, J. R., Vol. 16, 445–489. Mineral. Soc. Amer., Rev. Mineral.
87. Valley, J. W., and O'Neil, J. R., 1984. Fluid heterogeneity during granulite facies metamorphism in the Adirondacks:Stable isotope evidence. Contrib. Mineral. Petrol., 85:158–173.
88. van Roermund, H. L. M., and Drury, M. R., 1998. Ultra-high pressure (P>6 GPa) garnet peridotites in western Norway:Exhumation of mantle rocks from >185 km depth. Terra Nova, 10:295–301.
89. Wang, X., Zhang, R., and Liou, J. G., 1995. “ UHPM terrane in East Central China ”. In Ultrahigh pressure metamorphism, Edited by:Coleman, R. G., and Wang, X., 356–390. Cambridge, UK:Cambridge Univ. Press.
90. 2O at 1 GPa, with implications for mass transport in the crust and upper mantle. Contrib. Mineral. Petrol., 130:66–80.
91. Xu, J., 1993. “ Basic characteristics and tectonic evolution of the Tanchung-Lujiang fault zone ”. In The Tancheng-Lujiang wrench fault system, Edited by:Xu, J., 17–50. New York:John Wiley and Sons.
92. Yui, T. F., Rumble, D., Chen, C. H., and Lo, C. H., 1997. Stable isotope characteristics of eclogites from the ultra-high-pressure metamorphic terrain, east-central China. Chem. Geol., 137:135–147.
93. 18O ultrahigh-pressure metamorphic rocks from the Sulu terrain, eastern China. Geochim. et Cosmochim. Acta, 59:2859–2864.
94. 18O, ultrahigh-P garnet-bearing mafic and ultramafic rocks from Dabie Shan, China. Chem. Geol., 150:161–170.
95. l8O depletion in eclogite from the Su-Lu terrane in east China. Eur. Jour. Mineral., 8:317–323.
96. Zheng, Y. F., Fu, B., Gong, B., and Wang, Z. R., 1998. Carbon isotope anomaly in marbles associated with eclogites from the Dabie Mountains in China. Jour. Geol., 106:97–104.
97. Zheng, Y. F., Fu, B., Li, Y., Xiao, Y., and Li, S., 1998. Oxygen and hydrogen isotope geochemistry of ultra-high-pressure eclogites from the Dabie Mountains and the Sulu terrane. Earth Planet. Sci. Lett., 155:113–129.
98. Zheng, Y. F., Fu, B., Xiao, Y., Li, Y., and Gong, B., 1999. Hydrogen and oxygen isotope evidence for fluid-rock interactions in the stages of pre- and post-UHP metamorphism in the Dabie Mountains. Lithos, 46:677–693.