Auer, S., Bindeman, I., Wallace, P., Ponomareva, V., and Portnyagin, M.: The
origin of hydrous, high-
δ18O voluminous volcanism: diverse
oxygen isotope values and high magmatic water contents within the volcanic
record of Klyuchevskoy volcano, Kamchatka, Russia, Contrib.
Mineral. Petr., 157, 209–230,
https://doi.org/10.1007/s00410-008-0330-0, 2009.
Barnes, J. D. and Straub, S. M.: Chorine stable isotope variations in Izu
Bonin tephra: implications for serpentinite subduction, Chem. Geol.,
272, 62–74, https://doi.org/10.1016/j.chemgeo.2010.02.005, 2010.
Barnicoat, A. C. and Cartwright, I.: Focused fluid flow during subduction:
oxygen isotope data from high-pressure ophiolites of the western Alps, Earth
Planet. Sc. Lett., 132, 53–61,
https://doi.org/10.1016/0012-821X(95)00040-J, 1995.
Baumgartner, L. P. and Valley, J. W.: Stable isotope transport and contact
metamorphic fluid flow, Rev. Mineral. Geochem., 43,
415–467, https://doi.org/10.2138/gsrmg.43.1.415, 2001.
Baxter, E. F. and Caddick, M. J.: Garnet growth as a proxy for progressive
subduction zone dehydration, Geology, 41, 643–646,
https://doi.org/10.1130/G34004.1, 2013.
Bebout, G. E., Agard, P., Kobayashi, K., Moriguti, T., and Nakamura, E.:
Devolatilization history and trace element mobility in deeply subducted
sedimentary rocks: Evidence from Western Alps HP/UHP suites, Chem.
Geol., 342, 1–20, https://doi.org/10.1016/j.chemgeo.2013.01.009, 2013.
Bostock, M. G., Hyndman, R. D., Rondenay, S., and Peacock, S. M.: An inverted
continental Moho and serpentinization of the forearc mantle, Nature,
417, 536–538, https://doi.org/10.1038/417536a, 2002.
Bowman, J. R., Willett, S. D., and Cook, S. J.: Oxygen isotopic transport and
exchange during fluid flow: One-dimensional models and applications,
Am. J. Sci., 294, 1–55, https://doi.org/10.2475/ajs.294.1.1,
1994.
Bulle, F., Rubatto, D., Ruggieri, G., Luisier, C., Villa, I. M., and
Baumgartner, L.: Episodic hydrothermal alteration recorded by microscale
oxygen isotope analysis of white mica in the Larderello-Travale Geothermal
Field, Italy, Chem. Geol., 532, 119288,
https://doi.org/10.1016/j.chemgeo.2019.119288, 2019.
Caddick, M. J., Konopásek, J., and Thompson, A. B.: Preservation of
garnet growth zoning and the duration of prograde metamorphism, J.
Petrol., 51, 2327–2347, https://doi.org/10.1093/petrology/egq059,
2010.
Cartwright, I. and Barnicoat, A. C.: Stable isotope geochemistry of Alpine
ophiolites: a window to ocean-floor hydrothermal alteration and constraints
on fluid–rock interaction during high-pressure metamorphism, Int.
J. Earth Sci., 88, 219–235,
https://doi.org/10.1007/s005310050261, 1999.
Cartwright, I. and Barnicoat, A. C.: Geochemical and stable isotope
resetting in shear zones from Täschalp: constraints on fluid flow during
exhumation in the Western Alps, J. Metamorph. Geol., 21,
143–161, https://doi.org/10.1046/j.1525-1314.2003.00423.x, 2003.
Cook-Kollars, J., Bebout, G. E., Collins, N. C., Angiboust, S., and Agard,
P.: Subduction zone metamorphic pathway for deep carbon cycling: I. Evidence
from HP/UHP metasedimentary rocks, Italian Alps, Chem. Geol., 386,
31–48, https://doi.org/10.1016/j.chemgeo.2014.07.013, 2014.
de Capitani, C. and Brown, T. H.: The computation of chemical equilibrium in
complex systems containing non-ideal solutions, Geochim. Cosmochim.
Ac., 51, 2639–2652, https://doi.org/10.1016/0016-7037(87)90145-1,
1987.
de Capitani, C. and Petrakakis, K.: The computation of equilibrium
assemblage diagrams with Theriak/Domino software, Am. Mineral.,
95, 1006–1016, https://doi.org/10.2138/am.2010.3354, 2010.
Diener, J. F. A., Powell, R., White, R. W., and Holland, T. J. B.: A new
thermodynamic model for clino-and orthoamphiboles in the system
Na2O–CaO–FeO–MgO–
Al2O3–
SiO2–
H2O–O, J. Metamorph. Geol.,
25, 631–656, https://doi.org/10.1111/j.1525-1314.2007.00720.x, 2007.
Dorendorf, F., Wiechert, U., and Wörner, G.: Hydrated sub-arc mantle: a
source for the Kluchevskoy volcano, Kamchatka/Russia, Earth Planet.
Sc. Lett., 175, 69–86,
https://doi.org/10.1016/S0012-821X(99)00288-5, 2000.
Dubacq, B., Vidal, O., and De Andrade, V.: Dehydration of dioctahedral
aluminous phyllosilicates: thermodynamic modelling and implications for
thermobarometric estimates, Contrib. Mineral. Petr.,
159, 159–174, https://doi.org/10.1007/s00410-009-0421-6, 2010.
Eiler, J. M.: Oxygen isotope variations of basaltic lavas and upper mantle
rocks, Rev. Mineral. Geochem., 43, 319–364,
https://doi.org/10.2138/gsrmg.43.1.319, 2001.
Eiler, J. M., Farley, K. A., Valley, J. W., Hauri, E., Craig, H., Hart, S.
R., and Stolper, E. M.: Oxygen isotope variations in ocean island basalt
phenocrysts, Geochim. Cosmochim. Ac., 61, 2281–2293,
https://doi.org/10.1016/S0016-7037(97)00075-6, 1997.
Eiler, J. M., McInnes, B., Valley, J. W., Graham, C. M., and Stolper, E. M.:
Oxygen isotope evidence for slab-derived fluids in the sub-arc mantle,
Nature, 393, 777–781, https://doi.org/10.1038/31679, 1998.
Engi, M., Giuntoli, F., Lanari, P., Burn, M., Kunz, B., and Bouvier, A.-S.:
Pervasive Eclogitization Due to Brittle Deformation and Rehydration of
Subducted Basement: Effects on Continental Recycling?, Geochem.
Geophy. Geosy., 19, 865–881,
https://doi.org/10.1002/2017GC007215, 2018.
Errico, J. C., Barnes, J. D., Strickland, A., and Valley, J. W.: Oxygen
isotope zoning in garnets from Franciscan eclogite blocks: evidence for
rock–buffered fluid interaction in the mantle wedge, Contrib.
Mineral. Petr., 166, 1161–1176,
https://doi.org/10.1007/s00410-013-0915-0, 2013.
Evans, T. P.: A method for calculating effective bulk composition
modification due to crystal fractionation in garnet-bearing schist:
implications for isopleth thermobarometry, J. Metamorph. Geol.,
22, 547–557, https://doi.org/10.1111/j.1525-1314.2004.00532.x, 2004.
Ferry, J. M. and Spear, F. S.: Experimental calibration of the partitioning
of Fe and Mg between biotite and garnet, Contrib. Mineral.
Petr., 66, 113–117, https://doi.org/10.1007/BF00372150, 1978.
Ferry, J. M., Kitajima, K., Strickland, A., and Valley, J. W.: Ion microprobe
survey of the grain-scale oxygen isotope geochemistry of minerals in
metamorphic rocks, Geochim. Cosmochim. Ac., 144, 403–433,
https://doi.org/10.1016/j.gca.2014.08.021, 2014.
Frey, M., de Capitani, C., and Liou, J. G.: A new petrogenetic grid for
low-grade metabasites, J. Metamorph. Geol., 9, 497–509,
https://doi.org/10.1111/j.1525-1314.1991.tb00542.x, 1991.
Frezzotti, M. L., Selverstone, J., Sharp, Z. D., and Compagnoni, R.:
Carbonate dissolution during subduction revealed by diamond-bearing rocks
from the Alps, Nat. Geosci., 4, 703–706,
https://doi.org/10.1038/ngeo1246, 2011.
Friedman, I. and O'Neil, J. R.: Compilation of stable isotope fractionation factors of geochemical interest, in: Data of Geochemistry, 6th Edn., Geological Survey Professional Paper 440 KK,
https://pubs.usgs.gov/pp/0440kk/report.pdf, 1977.
Früh-Green, G. L., Scambelluri, M., and Vallis, F.: O–H isotope ratios
of high pressure ultramafic rocks: implications for fluid sources and
mobility in the subducted hydrous mantle, Contrib. Mineral.
Petr., 141, 145–159, https://doi.org/10.1007/s004100000228, 2001.
Gale, A., Dalton, C. A., Langmuir, C. H., Su, Y., and Schilling, J.-G.: The
mean composition of ocean ridge basalts, Geochem. Geophy.
Geosy., 14, 489–518, https://doi.org/10.1029/2012GC004334, 2013.
Gauthiez-Putallaz, L., Rubatto, D., and Hermann, J.: Dating prograde fluid
pulses during subduction by in situ U–Pb and oxygen isotope analysis,
Contrib. Mineral. Petr., 171, 1–20,
https://doi.org/10.1007/s00410-015-1226-4, 2016.
Gerdes, M. L., Baumgartner, L. P., Person, M., and Rumble, D.: One-and
two-dimensional models of fluid flow and stable isotope exchange at an
outcrop in the Adamello contact aureole, Southern Alps, Italy, Am.
Mineral., 80, 1004–1019,
https://doi.org/10.2138/am-1995-9-1016, 1995a.
Gerya, T. V., Stöckhert, B., and Perchuk, A. L.: Exhumation of
high-pressure metamorphic rocks in a subduction channel: A numerical
simulation, Tectonics, 21, 6–1, https://doi.org/10.1029/2002TC001406,
2002.
Giuntoli, F., Lanari, P., and Engi, M.: Deeply subducted continental fragments – Part 1: Fracturing, dissolution–precipitation, and diffusion processes recorded by garnet textures of the central Sesia Zone (western Italian Alps), Solid Earth, 9, 167–189, https://doi.org/10.5194/se-9-167-2018, 2018.
Gorman, P. J., Kerrick, D. M., and Connolly, J. A. D.: Modeling open system
metamorphic decarbonation of subducting slabs, Geochem. Geophy.
Geosy., 7, 1–21, https://doi.org/10.1029/2005GC001125, 2006.
Gregory, R. T. and Taylor Jr., H. P.: An oxygen isotope profile in a section
of Cretaceous oceanic crust, Samail ophiolite, Oman: Evidence for
δ18O buffering of the oceans by deep (> 5 km)
seawater-hydrothermal circulation at mid-ocean ridges, J.
Geophys. Res.-Sol. Ea., 86, 2737–2755,
https://doi.org/10.1029/JB086iB04p02737, 1981.
Hacker, B. R.:
H2O subduction beyond arcs, Geochem. Geophy.
Geosy., 9, 1–24, https://doi.org/10.1029/2007GC001707, 2008.
Hermann, J., Müntener, O., and Scambelluri, M.: The importance of
serpentinite mylonites for subduction and exhumation of oceanic crust,
Tectonophysics, 327, 225–238,
https://doi.org/10.1016/S0040-1951(00)00171-2, 2000.
Hernández-Uribe, D. and Palin, R. M.: A revised petrological model for
subducted oceanic crust: insights from phase equilibrium modelling, J. Metamorph. Geol., 37, 475–768, https://doi.org/10.1111/jmg.12483, 2019.
Heuret, A. and Lallemand, S.: Plate motions, slab dynamics and back-arc
deformation, Phys. Earth Planet. Int., 149,
31–51, https://doi.org/10.1016/j.pepi.2004.08.022, 2005.
Higashino, F., Rubatto, D., Kawakami, T., Bouvier, A.-S., and Baumgartner, L.
P.: Oxygen isotope speedometry in granulite facies garnet recording
fluid/melt–rock interaction (Sør Rondane Mountains, East Antarctica),
J. Metamorph. Geol., 37, 1037–1048,
https://doi.org/10.1111/jmg.12490, 2018.
Hirauchi, K. and Katayama, I.: Rheological contrast between serpentine
species and implications for slab–mantle wedge decoupling, Tectonophysics,
608, 545–551, https://doi.org/10.1016/j.tecto.2013.08.027, 2013.
Hoefs, J.: Stable isotope geochemistry, 7th Edn., Springer International Publishing, Switzerland, 389 pp., https://doi.org/10.1007/978-3-319-19716-6, 2015.
Holland, T. and Powell, R.: Thermodynamics of order-disorder in minerals;
II, Symmetric formalism applied to solid solutions, Am. Mineral.,
81, 1425–1437, https://doi.org/10.2138/am-1996-11-1215, 1996.
Holland, T. and Powell, R.: Activity–composition relations for phases in
petrological calculations: an asymmetric multicomponent formulation,
Contrib. Mineral. Petr., 145, 492–501,
https://doi.org/10.1007/s00410-003-0464-z, 2003.
Holland, T., Baker, J., and Powell, R.: Mixing properties and
activity-composition relationships of chlorites in the system
MgO-FeO-Al
2O
3-
SiO2-
H2O, Eur. J. Mineral., 10,
395–406, https://doi.org/10.1127/ejm/10/3/0395, 1998.
Holland, T. J. B. and Powell, R.: An internally consistent thermodynamic
data set for phases of petrological interest, J. Metamorph.
Geol., 16, 309–343, https://doi.org/10.1111/j.1525-1314.1998.00140.x,
1998.
Iwamori, H.: Transportation of
H2O and melting in subduction zones,
Earth Planet. Sc. Lett., 160, 65–80,
https://doi.org/10.1016/S0012-821X(98)00080-6, 1998.
John, T., Scambelluri, M., Frische, M., Barnes, J. D., and Bach, W.:
Dehydration of subducting serpentinite: implications for halogen mobility in
subduction zones and the deep halogen cycle, Earth Planet. Sc.
Lett., 308, 65–76, https://doi.org/10.1016/j.epsl.2011.05.038,
2011.
Kerrick, D. M. and Connolly, J. A. D.: Metamorphic devolatilization of
subducted marine sediments and the transport of volatiles into the Earth's
mantle, Nature, 411, 293–296, https://doi.org/10.1038/35077056, 2001.
Kohn, M. J.: Modeling of prograde mineral
δ18O changes in
metamorphic systems, Contrib. Mineral. Petr., 113,
249–261, https://doi.org/10.1007/BF00283232, 1993.
Konrad-Schmolke, M., O'Brien, P. J., de Capitani, C., and Carswell, D. A.:
Garnet growth at high-and ultra-high pressure conditions and the effect of
element fractionation on mineral modes and composition, Lithos, 103,
309–332, https://doi.org/10.1016/j.lithos.2007.10.007, 2008.
Konrad-Schmolke, M., Zack, T., O'Brien, P., and Barth, M.: Fluid migration
above a subducted slab – Thermodynamic and trace element modelling of
fluid–rock interaction in partially overprinted eclogite-facies rocks
(Sesia Zone, Western Alps), Earth Planet. Sc. Lett., 311,
287–298, https://doi.org/10.1016/j.epsl.2011.09.025, 2011.
Kuhn, B. K., Reusser, E., Powell, R., and Günther, D.: Metamorphic
evolution of calc-schists in the Central Alps, Switzerland, Schweiz.
Miner. Petrog., 85, 175–190,
https://doi.org/10.5169/seals-1659, 2005.
Lanari, P. and Duesterhoeft, E.: Modeling Metamorphic Rocks Using
Equilibrium Thermodynamics and Internally Consistent Databases: Past
Achievements, Problems and Perspectives, J. Petrol., 60,
19–56, https://doi.org/10.1093/petrology/egy105, 2019.
Lanari, P. and Engi, M.: Local bulk composition effects on metamorphic
mineral assemblages, Rev. Mineral. Geochem., 83
, 55–102,
https://doi.org/10.2138/rmg.2017.83.3, 2017.
Lanari, P. and Vho, A.: Fractionation of oxygen isotopes between minerals: a powerful tool for thermometry and investigating fluid-rock interaction, available at:
http://oxygen.petrochronology.org, last access: January 2020.
Lanari, P., Giuntoli, F., Loury, C., Burn, M., and Engi, M.: An inverse
modeling approach to obtain P–T conditions of metamorphic stages involving
garnet growth and resorption, Eur. J. Mineral., 29,
181–199, https://doi.org/10.1127/ejm/2017/0029-2597, 2017.
Laurent, V., Lanari, P., Naïr, I., Augier, R., Lahfid, A., and Jolivet,
L.: Exhumation of eclogite and blueschist (Cyclades, Greece):
Pressure–temperature evolution determined by thermobarometry and garnet
equilibrium modelling, J. Metamorph. Geol., 36, 769–798,
https://doi.org/10.1111/jmg.12309, 2018.
Liou, J. G., Tsujimori, T., Zhang, R. Y., Katayama, I., and Maruyama, S.:
Global UHP metamorphism and continental subduction/collision: the Himalayan
model, Int. Geol. Rev., 46, 1–27,
https://doi.org/10.2747/0020-6814.46.1.1, 2004.
Manning, C. E.: The chemistry of subduction-zone fluids, Earth Planet.
Sc. Lett., 223, 1–16,
https://doi.org/10.1016/j.epsl.2004.04.030, 2004.
Martin, L. A., Rubatto, D., Crépisson, C., Hermann, J., Putlitz, B., and
Vitale-Brovarone, A.: Garnet oxygen analysis by SHRIMP-SI: Matrix
corrections and application to high-pressure metasomatic rocks from Alpine
Corsica, Chem. Geol., 374, 25–36,
https://doi.org/10.1016/j.chemgeo.2014.02.010, 2014.
Mattey, D., Lowry, D., and Macpherson, C.: Oxygen isotope composition of
mantle peridotite, Earth Planet. Sc. Lett., 128, 231–241,
https://doi.org/10.1016/0012-821X(94)90147-3, 1994.
Mével, C.: Serpentinization of abyssal peridotites at mid-ocean ridges,
C. R. Geosci., 335, 825–852,
https://doi.org/10.1016/j.crte.2003.08.006, 2003.
Miller, J. A. and Cartwright, I.: Distinguishing between seafloor alteration
and fluid flow during subduction using stable isotope geochemistry: examples
from Tethyan ophiolites in the Western Alps, J. Metamorph. Geol.,
18, 467–482, https://doi.org/10.1046/j.1525-1314.2000.00274.x, 2000.
Miller, J. A., Cartwright, I., Buick, I. S., and Barnicoat, A. C.: An
O-isotope profile through the HP–LT Corsican ophiolite, France and its
implications for fluid flow during subduction, Chem. Geol., 178,
43–69, https://doi.org/10.1016/S0009-2541(00)00428-9, 2001.
Nakakuki, T. and Mura, E.: Dynamics of slab rollback and induced back-arc
basin formation, Earth Planet. Sc. Lett., 361, 287–297,
https://doi.org/10.1016/j.epsl.2012.10.031, 2013.
O'Neil, J. R. and Adami, L. H.: Oxygen isotope partition function ratio of
water and the structure of liquid water, J. Phys. Chem.,
73, 1553–1558, https://pubs.acs.org/doi/pdf/10.1021/j100725a062, 1969.
Padrón-Navarta, J. A., Hermann, J., Garrido, C. J.,
Sánchez-Vizcaíno, V. L., and Gómez-Pugnaire, M. T.: An
experimental investigation of antigorite dehydration in natural
silica-enriched serpentinite, Contrib. Mineral. Petr.,
159, 25–42, https://doi.org/10.1007/s00410-009-0414-5, 2010.
Padrón-Navarta, J. A., Sánchez-Vizcaíno, V. L., Hermann, J.,
Connolly, J. A., Garrido, C. J., Gómez-Pugnaire, M. T., and Marchesi, C.:
Tschermak's substitution in antigorite and consequences for phase relations
and water liberation in high-grade serpentinites, Lithos, 178, 186–196,
https://doi.org/10.1016/j.lithos.2013.02.001, 2013.
Page, F. Z., Kita, N. T., and Valley, J. W.: Ion microprobe analysis of
oxygen isotopes in garnets of complex chemistry, Chem. Geol.,
270, 9–19, https://doi.org/10.1016/j.chemgeo.2009.11.001, 2010.
Page, F. Z., Essene, E. J., Mukasa, S. B., and Valley, J. W.: A
garnet–zircon oxygen isotope record of subduction and exhumation fluids
from the Franciscan Complex, California, J. Petrol., 55,
103–131, https://doi.org/10.1093/petrology/egt062, 2013.
Page, F. Z., Cameron, E. M., Flood, C. M., Dobbins, J. W., Spicuzza, M. J.,
Kitajima, K., Strickland, A., Ushikubo, T., Mattinson, C. G., and Valley, J.
W.: Extreme oxygen isotope zoning in garnet and zircon from a metachert
block in mélange reveals metasomatism at the peak of subduction
metamorphism, Geology, 47, 655–658, https://doi.org/10.1130/G46135.1,
2019.
Parra, T., Vidal, O., and Agard, P.: A thermodynamic model for Fe–Mg
dioctahedral K white micas using data from phase-equilibrium experiments and
natural pelitic assemblages, Contrib. Mineral. Petr.,
143, 706–732, https://doi.org/10.1007/s00410-002-0373-6, 2002.
Peacock, S. A.: Fluid processes in subduction zones, Science, 248,
329–337, https://doi.org/10.1126/science.248.4953.329, 1990.
Peacock, S. M.: The importance of blueschist
→ eclogite dehydration
reactions in subducting oceanic crust, Geol. Soc. Am.
Bull., 105, 684–694, 1993.
Penniston-Dorland, S. C., Kohn, M. J., and Manning, C. E.: The global range
of subduction zone thermal structures from exhumed blueschists and
eclogites: Rocks are hotter than models, Earth Planet. Sc. Lett., 428, 243–254, https://doi.org/10.1016/j.epsl.2015.07.031, 2015.
Piccoli, F., Vitale Brovarone, A., Beyssac, O., Martinez, I., Ague, J. J.,
and Chaduteau, C.: Carbonation by fluid–rock interactions at high-pressure
conditions: implications for carbon cycling in subduction zones, Earth Planet. Sc. Lett., 445, 146–159,
https://doi.org/10.1016/j.epsl.2016.03.045, 2016.
Plank, T.: The chemical composition of subducting sediments, Treatise on
Geochemistry, 4, 607–629,
https://doi.org/10.1016/B978-0-08-095975-7.00319-3, 2014.
Plank, T. and Langmuir, C. H.: The chemical composition of subducting
sediment and its consequences for the crust and mantle, Chem. Geol.,
145, 325–394, https://doi.org/10.1016/S0009-2541(97)00150-2, 1998.
Poli, S. and Schmidt, M. W.: Petrology of subducted slabs, Annu. Rev.
Earth Pl. Sc., 30, 207–235,
https://doi.org/10.1146/annurev.earth.30.091201.140550, 2002.
Putlitz, B., Matthews, A. M., and Valley, J. W.: Oxygen and hydrogen isotope
study of high-pressure metagabbros and metabasalts (Cyclades, Greece):
implications for the subduction of oceanic crust, Contrib. Mineral. Petr., 138, 114–126,
https://doi.org/10.1007/s004100050012, 2000.
Rubatto, D. and Angiboust, S.: Oxygen isotope record of oceanic and
high-pressure metasomatism: a P–T–time–fluid path for the Monviso
eclogites (Italy), Contrib. Mineral. Petr., 170, 1–16,
https://doi.org/10.1007/s00410-015-1198-4, 2015.
Rumble, D.: Stable isotope fractionation during metamorphic devolatilization
reactions, Rev. Mineral. Geochem., 10, 327–353, 1982.
Russell, A. K., Kitajima, K., Strickland, A., Medaris, L. G., Schulze, D. J.,
and Valley, J. W.: Eclogite-facies fluid infiltration: constraints from
δ18O zoning in garnet, Contrib. Mineral. Petr., 165, 103–116, https://doi.org/10.1007/s00410-012-0794-9,
2013.
Scambelluri, M., Fiebig, J., Malaspina, N., Müntener, O., and Pettke, T.:
Serpentinite subduction: implications for fluid processes and trace-element
recycling, Int. Geol. Rev., 46, 595–613,
https://doi.org/10.2747/0020-6814.46.7.595, 2004.
Schmidt, M. W. and Poli, S.: 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. Sc. Lett., 124, 105–118, https://doi.org/10.1016/0012-821X(94)00080-8,
1994.
Sharp, Z.: Principles of stable isotope geochemistry, 2nd Edn., University of New Mexico, 384 pp.,
https://doi.org/10.25844/h9q1-0p82, 2017.
Sharp, Z. D. and Barnes, J. D.: Water-soluble chlorides in massive seafloor
serpentinites: a source of chloride in subduction zones, Earth Planet. Sc. Lett., 226, 243–254,
https://doi.org/10.1016/j.epsl.2004.06.016, 2004.
Siron, G., Baumgartner, L., Bouvier, A.-S., Putlitz, B., and Vennemann, T.:
Biotite reference materials for secondary ion mass spectrometry
18O∕16O measurements, Geostand. Geoanal. Res.,
41, 243–253, https://doi.org/10.1111/ggr.12148, 2017.
Spandler, C. and Hermann, J.: High-pressure veins in eclogite from New
Caledonia; Implications for fluid migration and seismic activity in
subduction zones, Geochim. Cosmochim. Ac., Supplement, 69, A664,
https://ui.adsabs.harvard.edu/abs/2005GeCAS..69..664S/abstract,
2005.
Spear, F. S.: Metamorphic fractional crystallization and internal
metasomatism by diffusional homogenization of zoned garnets, Contrib. Mineral. Petr., 99, 507–517,
https://doi.org/10.1007/BF00371941, 1988.
Spear, F. S., Pattison, D. R. M., and Cheney, J. T.: The metamorphosis of
metamorphic petrology, in The Web of Geological Sciences: Advances, Impacts,
and Interactions II, Geol. Soc. Am., 523, 31–73, https://doi.org/10.1130/2016.2523(02), 2017.
Staudigel, H.: Chemical fluxes from hydrothermal alteration of the oceanic
crust, in: Treatise on Geochemistry, 2nd Edn., edited by: Turekian,
H. D. H. K., Elsevier, Oxford, UK, 583–606, 2014.
Staudigel, H., Plank, T., White, B., and Schmincke, H.-U.: Geochemical fluxes
during seafloor alteration of the basaltic upper oceanic crust: DSDP Sites
417 and 418, Subduction: top to bottom, 96, 19–38,
https://doi.org/10.1029/GM096p0019, 1996.
Stern, R. J.: Subduction zones, Rev. Geophys., 40, 1–40,
https://doi.org/10.1029/2001RG000108, 2002.
Sun, S.-S. and McDonough, W. F.: Chemical and isotopic systematics of
oceanic basalts: implications for mantle composition and processes,
Geol. Soc., London, Special Publications, 42, 313–345,
https://doi.org/10.1144/GSL.SP.1989.042.01.19, 1989.
Syracuse, E. M., van Keken, P. E., and Abers, G. A.: The global range of
subduction zone thermal models, Phys. Earth Planet.
Int., 183, 73–90, https://doi.org/10.1016/j.pepi.2010.02.004,
2010.
Tracy, R. J.: Compositional zoning and inclusions in metamorphic minerals.
Characterization of Metamorphism through Mineral Equilibria, Rev.
Mineral., 10, 355–397, 1982.
Valley, J.: Stable isotope geochemistry of metamorphic rocks, Rev.
Mineral. Geochem., 16, 445–489, 1986.
Vho, A., Lanari, P., and Rubatto, D.: An internally-consistent database for
oxygen isotope fractionation between minerals, J. Petrol.,
https://doi.org/10.1093/petrology/egaa001, 2020.
Vidal, O., Lanari, P., Munoz, M., Bourdelle, F., de Andrade, V., and Walker,
J.: Deciphering temperature, pressure and oxygen-activity conditions of
chlorite formation, Clay Miner., 51, 615–633,
https://doi.org/10.1180/claymin.2016.051.4.06, 2016.
Vielzeuf, D., Veschambre, M., and Brunet, F.: Oxygen isotope heterogeneities
and diffusion profile in composite metamorphic-magmatic garnets from the
Pyrenees, Am. Mineral., 90, 463–472,
https://doi.org/10.2138/am.2005.1576, 2005a.
Vielzeuf, D., Champenois, M., Valley, J. W., Brunet, F., and Devidal, J. L.:
SIMS analyses of oxygen isotopes: matrix effects in Fe–Mg–Ca garnets,
Chem. Geol., 223, 208–226,
https://doi.org/10.1016/j.chemgeo.2005.07.008, 2005b.
Wada, I., Wang, K., He, J., and Hyndman, R. D.: Weakening of the subduction
interface and its effects on surface heat flow, slab dehydration, and mantle
wedge serpentinization, J. Geophys. Res.-Sol. Ea.,
113, B04402, https://doi.org/10.1029/2007JB005190, 2008.
Walter, M. J.: Melting of garnet peridotite and the origin of komatiite and
depleted lithosphere, J. Petrol., 39, 29–60,
https://doi.org/10.1093/petroj/39.1.29, 1998.
White, W. M. and Klein, E. M.: Composition of the Oceanic Crust, Treatise on
Geochemistry, 2nd Edn., 4, 457–496,
https://doi.org/10.1016/B978-0-08-095975-7.00315-6, 2014.
Williams, M. J.: Tracing Fluids from Seafloor to Deep Subduction
Environments: An In-situ Geochemical Investigation of Fluid-Mobile Elements
in Oceanic Crust, Ph.D thesis, Australian National University, Canberra,
https://doi.org/10.25911/5d650de5b5cfd, 325 pp., 2019.
Zack, T. and John, T.: An evaluation of reactive fluid flow and trace
element mobility in subducting slabs, Chem. Geol., 239, 199–216,
https://doi.org/10.1016/j.chemgeo.2006.10.020, 2007.
Zheng, Y. F.: Oxygen isotope fractionation in metal monoxides, Mineral.
Mag., 58, 1000–1001, https://doi.org/10.1180/minmag.1994.58A.2.255, 1994.
