Abstract
Peak metamorphic temperatures for the coesite-pyrope-bearing whiteschists from the Dora Maira Massif, western Alps were determined with oxygen isotope thermometry. The δ18O(smow) values of the quartz (after coesite) (δ18O=8.1 to 8.6‰, n=6), phengite (6.2 to 6.4‰, n=3), kyanite (6.1‰, n=2), garnet (5.5 to 5.8‰, n=9), ellenbergerite (6.3‰, n=1) and rutile (3.3 to 3.6‰, n=3) reflect isotopic equilibrium. Temperature estimates based on quartz-garnet-rutile fractionation are 700–750 °C. Minimum pressures are 31–32 kb based on the pressure-sensitive reaction pyrope + coesite = kyanite + enstatite. In order to stabilize pyrope and coesite by the temperature-sensitive dehydration reaction talc+kyanite=pyrope+coesite+H2O, the a(H2O) must be reduced to 0.4–0.75 at 700–750 °C. The reduced a(H2O) cannot be due to dilution by CO2, as pyrope is not stable at X(CO2)>0.02 (T=750 °C; P=30 kb). In the absence of a more exotic fluid diluent (e.g. CH4 or N2), a melt phase is required. Granite solidus temperatures are ∼680 °C/30 kb at a(H2O)=1.0 and are calculated to be ∼70°C higher at a(H2O)=0.7, consistent with this hypothesis. Kyanite-jadeite-quartz bands may represent a relict melt phase. Peak P-T-f(H2O) estimates for the whiteschist are 34±2 kb, 700–750 °C and 0.4–0.75. The oxygen isotope fractionation between quartz (δ18O=11.6‰) and garnet (δ18O=8.7‰) in the surrounding orthognesiss is identical to that in the coesitebearing unit, suggesting that the two units shared a common, final metamorphic history. Hydrogen isotope measurements were made on primary talc and phengite (δD(SMOW)=-27 to-32‰), on secondary talc and chlorite rite after pyrope (δD=-39 to -44‰) and on the surrounding biotite (δD=-64‰) and phengite (δD=-44‰) gneiss. All phases appear to be in nearequilibrium. The very high δD values for the primary hydrous phases is consistent with an initial oceanicderived/connate fluid source. The fluid source for the retrograde talc+chlorite after pyrope may be fluids evolved locally during retrograde melt crystallization. The similar δD, but dissimilar δ18O values of the coesite bearing whiteschists and hosting orthogneiss suggest that the two were in hydrogen isotope equilibrium, but not oxygen isotope equilibrium. The unusual hydrogen and oxygen isotope compositions of the coesite-bearing unit can be explained as the result of metasomatism from slab-derived fluids at depth.
Similar content being viewed by others
References
Agrinier P (1991) The natural calibration of 18O/16O geothermometers: application to the quartz-rutile mineral pair. Chem Geol 91: 49–64
Baker AJ (1990) Stable isotopic evidence for fluid-rock interactions in the Ivrea Zone, Italy, J Petrol 31: 243–260
Berman RG (1988) Internally-consistent thermodynamic data for minerals in the system Na2O-K2O-Ca-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2. J Petrol 29: 445–522
Black PM (1974) Oxygen isotope study of metamorphic rocks from the Ouégoa District, New Caledonia. Contrib Mineral Petrol 47: 197–206
Boettcher AL, Wyllie PJ (1968) Melting of granite with excess water to 30 kilobars pressures. J Geol 76: 235–244
Bottinga Y, Javoy M (1975) Oxygen isotope partitioning among the minerals in igneous and metamorphic rocks. Rev Geophys Space Phys 13: 401–418
Brown EH, O'Neil JR (1982) Oxygen isotope geothermometry and stabilty of lawsonite and pumpellyite in the Shuksan Suite, North Cascades, Washington. Contrib Mineral Petrol 80: 240–244
Burkhard M, Kerrich R (1988) Fluid regimes in the deformation of the Helvetic nappes, Switzerland, as inferred from stable isotope data. Contrib Mineral Petrol 99: 416–429
Burnham CW (1979) The importance of volatile constituents. In: Yoder HS Jr (ed) The evolution of the igneous rocks: Fiftieth Anniversry perspectives. Princeton University Press, Princeton, pp. 902–940
Chesnokov BV, Popov VA (1965) Increase in the volume of quartz grains in South Urals eclogite. Dokl Akad Nauk SSSR 162: 176–178
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
Chopin C (1985) Les relations de phases dans les métapelites de haute pression: approaches expérimentale et naturaliste, conséquences géodynamiques pour les Alpes occidentales. Thèse d'état, Université de Paris 6, Paris
Chopin C (1986) Phase relationships of ellenbergerite, a new highpressure Mg-Al-Ti-silicate in pyrope-coestite-quartzite from the Western Alps. Geol Soc Am Mem 164: 31–42
Chopin C (1987) Very-high-pressure metamorphism in the western Alps: implications for subduction of continental crust. Philos Trans R Soc London A 321: 183–197
Chopin C, Henry C, Michard A (1991) Geology and petrology of the coesite-bearing terrain, Dora Maira massif, Western Alps. Eur J Mineral 3: 263–291
Desmons J, O'Neil JR (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
Enami M, Zang Q (1990) Quartz pseudomorphs after coesite in eclogites from Shandong Province, east China. Am Mineral 75: 381–386
Essene EJ (1989) The current status of thermobarometry in metamorphic rocks. In: Daly JS, Cliff RA, Yardley BWD (eds) Evolution of metamorphic rocks. Geol Soc Spec Publ 43: 1–44
Farver JR, Yund RA (1991) Oxygen diffusion in quartz: dependence on temperature and water fugacity. Chem Geol 90: 55–70
Fourcade S, Javoy M (1973) Rapports 18O/16O dans les roches du vieux socle catazonal d'In Ouzzal (Sahara algérien). Contrib Mineral Petrol 42: 235–244
Frey M, Hunziker JC, O'Neil JR, Schwander HW (1976) Equilibrium-disequilibrium relations in the Monte Rosa granite, Western Alps: petrological, Rb-Sr and stable isotope data. Contrib Mineral Petrol 55: 147–179
Friedrichsen H, Morteani G (1979) Oxygen and hydrogen isotope studied on minerals from Alpine fissures and their gneissic host rocks, western Tauern Window (Austria). Contrib Mineral Petrl 70: 149–152
Garlick GD, Epstein S (1968) Oxygen isotope ratios in coexisting minerals of regionally metamorphosed rocks. Geochim Cosmochim Acta 31: 181–214
Gasparik T, Newton RC (1984) The reversed alumina contents of orthopyroxene in equilibrium with spinel and forsterite in the system MgO-Al2O3-SiO2. Contrib Mineral Petrol 85: 186–196
Graham CM (1981) Experimental hydrogen isotope studies III: diffusion of hydrogen in hydrous minerals, and stable isotope exchange in metamorphic rocks. Contrib Mineral Petrol 76: 216–228
Hirajima T, Ishiwatari A, Cong B, Zhang R, Bann S, Nozaka T (1991) Coesite from Mengzhong eclogite at Donghai county, northeastern Jiangsu province, China. Mineral Mag 54: 579–583
Hoernes S, Friedrichsen H (1974) Oxygen isotope studies on metamorphic rocks of the Western Hole Tauern Area (Austria). Schweiz Mineral Petrogr 54: 769–788
Hoernes S, Friedrichsen H (1978) Oxygen and hydrogen isotope study of the polymetamorphic area of the northern Ötztal-Stubai Alps (Tyrol). Contrib Mineral Petrol 67: 305–315
Hoernes S, Friedrichsen H (1980) Oxygen and hydrogen isotopic composition of Alpine and Pre-Alpine minerals of the Swiss Central Alps. Contrib Mineral Petrol 72: 19–32
Hoernes S, Hoffer E (1979) Equilibrium relations of prograde metamorphic mineral assemblages. A stable isotope study of rocks of the Damara Orogen, from Namibia. Contrib Mineral Petrol 68: 377–389
Hoernes S, van Reenen DD (1992) The oxygen-isotopic composition of granulites and retrogressed granulites from the Limpopo Belt as a monitor of fluid-rock interaction. Precamb Res 55: 353–364
Hoffbauer R, Hoernes S, Fiorentini E (1993) Oxygen isotope thermometry on granulite-grade rocks from Sri Lanka. Precamb Res (in press)
Holland TJB, Poweil R (1990) An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K2O-Na2O-CaO-MgO-MnO-FeO-Fe2O3-Al2O3-TiO2-SiO2-C-H2-O2. J Metam Geol 8: 89–124
Honma H, Sakai H (1975) Oxygen isotope study of metamorphic and granitic rocks of the Yanai District in the Ryoke Belt, Japan. Contrib Mineral Petrol 52: 107–120
Huang WL, Wyllie PJ (1975) Melting reactions in the system NaAlSi3O8-KAlSi3O8-SiO2 to 35 kilobars, dry and with excess water. J Geol 83: 737–748
Huebner M, Kyser TK, Nisbet EG (1986) Stable-isotope geochemistry of high-grade metapelites from the Central zone of the Limpopo belt. Am Mineral 71: 1343–1353
Janardhan AS, Newton RC, Smith JV (1979) Ancient crustal metamorphism at low p(H2O): charnockite formation at Kabbaldurga, South India. Nature 278: 511–514
Javoy M, Fourcade S, Allegre CJ (1970) Graphical method for examination of 18O/16O fractionations in silicate rocks. Earth Planet Sci Lett 10: 12–16
Jiang J, Clayton RN, Newton RC (1988) Fluids in granulite facies metamorphism: a comparative oxygen isotope study on the South India and Adirondacks high-grade terrains. J Geol 96: 517–533
Kawahata H, Kusakabe M, Kikuchi Y (1987) Strontium oxygen and hydrogen isotope geochemistry of hydrothermally altered and weathered rocks in DSDP Hole 504B, Costa Rica Rift Earth Planet Sci Lett 85: 343–355
Kennedy CS, Kennedy GC (1976) The equilibrium boundary between graphite and diamond. J Geophys Res 81: 2467–2470
Kesson SE, Ringwood AE (1989) Slab-mantle interactions 1. Sheared and refertilised garnet peridotite xenoliths-samples of the Wadati-Benioff zones? Chem Geol 78: 83–96
Kienast JR, Lombardo B, Biino G, Pinardon JL (1991) Petrology of very-high-pressure eclogite rocks from the Brossasco-Isasca complex, Dora-Maira Massif, Italian Western Alps. J Metam Geol 9: 19–34
Kitahara S, Takenouchi S, Kennedy GC (1966) Phase relations in the system MgO-SiO2-H2O at high temperatures and pressures. Am J Sci 264: 223–233
Kusakabe M, Shibata T, Yamamoto M, Mayeda S, Kagami H, Honma H, Masuda H, Sakai H (1989) 5. Petrology and isotope characteristics (H, O, S, Sr, and Nd) of basalts from ocean drilling program Hole 504B, Leg 111, Costa Rica Rift. In: Proceedings of the Ocean Drilling Program, scientific results 111: 47–60
Lichtenstein U, Hoernes S (1992) Oxygen isotope fractionation between grossular-spessartine garnet and water: an experimental investigation. Eur J Mineral 4: 239–249
Margaritz M, Taylor HP Jr (1976) Oxygen, hydrogen and carbon isotope studies of the Franciscan formation, Coast Ranges, California. Geochim Cosmochim Acta 40: 215–234
Massonne H-J (1983) Experiments on melting to 50 kbar in the system MgO-Al2O3-SiO2-H2O (MASH) with excess SiO2 and H2O. EOS 64: 875
Massonne H-J, Schreyer W (1986) High-pressure syntheses and X-ray properties of white micas in the system K2O-MgO-Al2O3-SiO2-H2O. Neues Jahrb Mineral (Abh) 153: 177–215
Massonne H-J, Schreyer W (1989) Stability field of the high-pressure assemblage talc + phengite and two new phengite barometers. Eur J Mineral 1: 391–410
Matthews A (1992) Oxygen isotope geothermometers for high pressure metamorphic rocks. In: Stable isotopes as tracers of metamorphic processes. Abstr Prog Internat Geol Correlation Prog 304: 30
Matthews A, Schliestedt M (1984) Evolution of the blueschist and greenschist facies rocks of Sifnos, Cyclades, Greece. A stable isotope study of subduction-related metamorphism. Contrib Mineral Petrol 88: 150–163
McCaig AM, Wickham SM, Taylor HP Jr (1990) Deep Fluid circulation in alpine shear zones, Pyrenees France: field and oxygen isotope studies. Contrib Mineral Petrol 106: 41–60
McKie D (1959) Yoderite, a new hydrous magnesium aluminosilicate from Mautia Hill, Tanganyika, Mineral. Mag 32: 282–307
McNaughton NJ, Wilson AF (1980) Problems in oxygen isotope geothermometry in mafic granulite facies rocks from near Einasleigh, Northern Queensland. Prec Camb Res 13: 77–86
Monié P, Chopin C (1991) 40Ar-39Ar dating in coesite-bearing and associated units of the Dora Maira massif, western Alps. Eur J Mineral 3: 239–262
Morikiyo T (1986) Hydrogen and carbon isotope studies on the graphite-bearing metapelites in the northern Kiso district of central Japan. Contrib Mineral Petrol 94: 165–177
Munz IA (1990) Whiteschists and orthoamphibole-cordierite rocks and the P-T-t path of the Modum Complex, South Nroway. Lithos 24: 181–200
Okay AI, Xu S, Sengor AMC (1989) Coesite from the Dabie Shan eclogites, central China. Eur J Mineral 1: 595–598
O'Neil JR, Ghent ED (1975) Stable isotope study of coexiting metamorphic minerals from the Esplanade Range, British Columbia. Geol Soc Am Bull 86: 1708–1712
O'Neil JR, Hay RL (1973) 18O/16O ratios in cherts associated with the saline lake deposits of East Africa. Earth Planet Sci Lett 19: 257–266
O'Neil JR, Kharaka YK (1976) Hydrogen and oxygen isotope exchange reactions between clay minerals and water. Geochim Cosmochim Acta 40: 241–246
Pacquette J-L, Chopin C, Peucat I-J (1989) U-Pb zircon, Rb-Sr and Sm-Nd geochronology of high to very-high-pressure meta-acidic rocks from the Western Alps. Contrib Mineral Petrol 101: 280–289
Perkins D III, Holland TJB, Newton RC (1981) The Al2O3 contents of enstatite in equilibrium with garnet in the system MgO-Al2O3-SiO2 at 15–40 kbar and 900°–1600°C. Contrib Mineral Petrol 78: 99–109
Perry EC Jr, Tan FC (1972) Significance of oxygen and carbon isotope variations in early Precambrian cherts and carbonate rocks of southern Africa. Geol Soc Am Bull 83: 647–664
Pineau F, Javoy M, Behar F, Touret J (1981) La géochimie isotopique du faciès granulite du Bamble (Norvège) et l'origine des fluides carbonés dans la croûte profonde. Bull Mineral 104: 630–641
Powell R, Holland TJB (1988) An internally consistent thermodynamic dataset with uncertainties and correlations: 3. Applications to geobarometry, worked examples and a computer program. J Metam Geol 6: 173–204
Reinecke T (1991) Very-high-pressure metamorphism and uplift of coesite-bearing metasediments from the Zermatt-Saas zone, Western Alps. Eur J Mineral 3: 7–17
Robert C, Javoy M, Kienast J-R (1985) Coefficients de distribution et mesures isotopiques 18O/16O comparisons thermométriques et barométriques sur quelques éclogites et micaschistes de la zone Sesia-Lanzo (Alpes italiennes). Bull Mineral 108: 699–711
Rossman GR, Beran A, Langer K (1989) The hydrous component of pyrope from the Dora Maira Massif, Western Alps. Eur J Mineral 1: 151–154
Rumble D III (1978) Mineralogy, petrology and oxygen isotope geochemistry of the Clough Formation, Black Mountain, Western New Hampshire, USA. J Petrol 19: 317–340
Rye RO, Schuiling RD, Rye DM, Hansen JBH (1976) Carbon, hydrogen, and oxygen isotope studies of the regional metamorphic complex at Naxos, Greece. Geochim Cosmochim Acta 40: 1031–1049
Savin SM (1980) Oxygen and hydrogen isotope effects in low-temperature mineral-water interactions. In: Fritz AP, Fontes JCh (eds) The terrestrial environment. Handbook of environmental isotope geochemistry, vol. 1. Elsevier, Amsterdam, pp. 283–327
Savin SM, Epstein S (1970) The oxygen and hydrogen isotope geochemistry of clay minerals. Geochim Cosmochim Acta 34: 25–42
Schertl H-P, Schreyer W, Chopin C (1991) The pyrope-coesite 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
Schmädicke E (1991) Quartz pseudomorphs after coesite in eclogites from the Saxonian Erzgebirge. Eur J Mineral 3: 231–238
Schreyer W (1977) Whiteschists: their compositions and pressuretemperature regimes based on experimental, field, and petrographic evidence. Tectonophysics 43: 127–144
Schreyer W, Massonne H-J, Chopin C (1987) Continental crust subducted to depths near 100 km: implications for magma and fluid genesis in colliston zones. In: Mysen BO (ed) Magmatic processes: physiochemical principles. Geochem Soc Spec Pub 1: 155–163
Schwarcz HP, Clayton RN, Mayeda T (1970) Oxygen isotopic studies of calcareous and pelitic metamorphic rocks, New England. Geol Soc Am Bull 81: 2299–2316
Sharp ZD (1990) A laser-based microanalytical method for the in situ determination of oxygen isotope ratios in silicates and oxides. Geochim Cosmochim Acta 54: 1353–1357
Sharp ZD (1992) In situ laser microprobe techniques for stable isotope analysis. Chem Geol 101: 3–19
Sharp ZD, O'Neil JR, Essene EJ (1988) Oxygen isotope variations in granulite-grade iron formations: constraints on oxygen diffusion and retrograde isotopic exchange. Contrib Mineral Petrol 98: 490–501
Sharp ZD, Giletti BJ, Yoder HS Jr (1991) Oxygen diffusion rates in quartz exchanged with CO2. Earth Planet Sci Lett 107: 339–348
Sharp ZD, Essene EJ, Smyth JR (1992) Ultra-high temperatures from oxygen isotope thermometry of a coesite-sanidine grospydite. Contrib Mineral Petrol 112: 358–370
Shutong X, Okav AI, Shouyuan J, Sengör AMC, Wen S, Yican L, Laili J (1992) Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting Science 256:80–82
Smith DC (1984) Coesite in clinopyroxene in the Caledonides and its implications for geodynamics. Nature 310: 641–644
Smith DC, Lappin MA (1987) Coesite in the Straumen kyaniteeclogite pod, Norway. Terra Res 1: 47–56
Sobolev NV, Shatsky VS (1990) Diamond inclusions in garnets from metamorphic rocks: a new environment for diamond formation. Nature 343: 742–745
Stakes DS (1991) Oxygen and hydrogen isotope compositions of oceanic plutonic rocks: High-temperature deformation and metamorphism of oceanic layer 3. In: Taylor HP JR, O'Neil JR, Kaplan IR (eds) Stable isotope geochemistry: a tribute to Samuel Epstein. The Geochemical Society Spec Pub 3: 77–90
Stern CR, Huang WL, Wyllie PJ (1975) Basalt-andesite-rhyolite-H2O: crystallization intervals with excess H2O and H2O-undersaturated liquidus surfaces to 35 kilobars, with implications for magma genesis. Earth Planet Sci Lett 28: 189–196
Suzuoki T, Epstein S (1976) Hydrogen isotope fractionation between OH-bearing minerals and water. Geochim Cosmochim Acta 40: 1229–1240
Tagiri M, Bakirov A (1990) Quartz pseudomorph after coesite in garnet from a garnet-chloritoid-talc schist, northern Tien-Shan, Kirghiz, SSR. Proc Japan Acad 66: 135–139
Tatsumi Y (1989) Migration of fluid phases and genesis of basalt magmas in subduction zones. J Geophys Res 94: 4697–4707
Taylor HP Jr (1974) The application of oxygen and hydrogen isotope studies to problems of hydrothermal alteration and ore deposition. Econ Geol 69: 843–883
Taylor HP Jr, Coleman RG (1968) O18/O16 ratios of coexisting minerals in glaucophane-bearing metamorphic rocks. Geol Soc Am Bull 79: 1727–1756
Taylor HP Jr, Epstein S (1962) Relationship between O18/O16 ratios in coexisting minerals of igneous and metamorphic rocks. Geol Soc Am Bull 73: 675–694
Taylor HP Jr, Albee AL, Epstein S (1963) O18/O16 ratios of coexisting minerals in three assemblages of kyanite-zone pelitic schist. J Geol 71: 513–522
Thomas LJ, Harmon RS, Oliver GJH (1985) Stable isotope composition of alteration fluids in low-grade lower Palaeozoic rocks, English Lake District. Mineral Mag 49: 425–434
Tilton GR, Schreyer W, Schertl H-P (1989) Pb-Sr-Nd isotopic behavior of deeply subducted crystal rocks from Dora Maira Massif, Western Alps, Italy. Geochim Cosmochim Acta 53: 1391–1400
Tilton GR, Schreyer W, Schertl H-P (1991) Pb-Sr-Nd isotopic behavior of deeply subducted crystal rocks from the Dora Maira Massif, Western Alps, Italy-II: what is the age of the ultrahigh-pressure metamorphism? Contrib Mineral Petrol 108: 22–33
Touret J (1971) Le facies granulite en Norvège méridionale. Lithos 4: 239–249
Vaidya SN, Beiley S, Pasternack T, Kennedy GC (1973) Compressibility of fifteen minerals to 45 kilobars. J Geophys Res 78: 6893–6898
Vallance TG (1967) Mafic rock alteration and isochemical development of some cordierite-anthophyllite rocks. J Petrol 8: 84–96
Valley JW (1986) Stable isotope geochemistry of metamorphic rocks. In: Valley JW, Taylor HP JR, O'Neil JR (eds) Stable isotopes in high temperature geological processes. Rev Mineral 16:445–489
Valley JW, O'Neil JR (1984) Fluid heterogeneity during granulite facies metamorphism in the Adirondacks: stable isotope evidence. Contrib Mineral Petrol 85: 158–173
Valley JW, Bohlen SR, Essene EJ, Lamb W (1990) Metamorphism in the Adirondacks II. The role of fluids. J Petrol 31: 555–596
Vennemann TW, O'Neil JR (1993) A simple and inexpensive method of hydrogen isotope analysis of minerals and rocks based on zinc reagent. Isotope Geosci (in press)
Vennemann TW, Smith HS (1992) Stable isotope profile across the orthoamphibole isograd in the Southern Marginal Zone of the Limpopo Belt, South Africa. Precamb Res 55: 365–397
Vialon P (1966) Etude géologique du massif cristallin Dora-Maira, Alpes cottiennes internes, Italie. Thèse d'état, Université de Grenoble
Vrána S (1975) Magnesian-aluminous rocks, the associated ore mineralization and the problem of magnesium-iron metasomatism. Krystallinikum 11: 101–114
Vrána S, Barr MWC (1972) Talc-kyanite-quartz schists and other high-pressure assemblages from Zambia. Mineral Mag 38: 837–846
Wang X, Liou JG, Mao HK (1989) Coesite-bearing eclogites from the Dabie Mountains in central China. Geol 17: 1085–1088
Whelan JF, Rye RO, DeLorraine W (1984) The Balmat-Edwards zinc-lead deposits-synsedimentary ore from Mississippi Valleytype fluids. Econ Geol 79: 239–265
Wickham SM, Taylor HP Jr (1985) Stable isotopic evidence for large-scale seawater infiltration in a regional metamorphic terrane; the Trois Seigneurs Massif, Pyrenees, France. Contrib Mineral Petrol 91: 122–137
Wilson AF, Green DC (1971) The use of oxygen isotopes for geothermometry of Proterozoic and Archaean granulites. Spec Publ Geol Soc Aust 3: 389–400
Wilson AF, Green DC, Davidson LR (1970) The use of oxygen isotope geothermometry on the granulites and related intrusives, Musgrave Ranges, Central Australia. Contrib Mineral Petrol 27: 166–178
Yang J, Smith DC (1989) Evidence for a former sanidine-coesite eclogite at Lanshantou, eastern China and the recognition of the Chinese “Su-Lu Coesite-eclogite Province”. Terra Abstra 1: 26
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Sharp, Z.D., Essene, E.J. & Hunziker, J.C. Stable isotope geochemistry and phase equilibria of coesite-bearing whiteschists, Dora Maira Massif, western Alps. Contr. Mineral. and Petrol. 114, 1–12 (1993). https://doi.org/10.1007/BF00307861
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00307861