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Subject:

Re: CO2 and granulites

From:

"Timo G. Nijland" <[log in to unmask]>

Reply-To:

Metamorphic Studies Group <[log in to unmask]>

Date:

Wed, 30 Oct 2002 19:32:16 +0100

Content-Type:

text/plain

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text/plain (274 lines)

Dear Bruno

Whether or not CO2 is important: See the short selection below

Cheers, Timo


Andersen, T., 1998. Fluid inclusions in Scourian granulites from the
Lewisian complex of NW Scotland: Evidence for CO2-rich fluid in late
Archaean high-grade metamorphism. Lithos 40:93-104.

Aranovich, L.Y. & Newton, R.C., 1999. Experimental determination of CO2 -
H2O activity - composition relations at 600 - 1000°C and 6 -14 kbar by
reversed decarbonation and dehydration reactions. Amer. Mineral.
84:1319-1332. 

Aranovich, L.Y., Shmulovich, K.I., & Fedkin, V.V. 1987. The H2O and CO2
regime in regional metamorphism. Geochem. Int. 29:1379-1401.

Baker, A.J. & Fallick, A.E., 1988. Evidence for CO2 infiltration in
granulite facies marbles from Lofoten - Vestrålen, Norway. EPSL 91:132-140. 

Bakker, R.J. & Jansen, J.B.H., 1993. Calculated fluid evolution path versus
fluid inclusion data in the COHN system as examplified by metamorphic rocks
from Rogaland, south?west Norway. J. Metam. Geol. 11:357?370. 

Bolder-Schrijver, L.J.A., Kriegsman, L.M. & Touret, J.L.R., 1997. Carbonate
/ CO2 inclusions in sapphirine-bearing granulites from Hakurutale, Sri
Lanka. In: Boiron, M.C. & Pironon, J., eds., Proceedings of the 14th
ECROFI, 46-47.

Bradshaw, J.Y., 1989. Early Creataceous vein-related garnet granulite in
Fiordland, southwest New Zealand: A case for infiltration of mantle-derived
CO2-rich fluids. J. Geol. 97:697-717.

Broekmans, M.A.T.M., Nijland, T.G. & Jansen, J.B.H., 1994. Are stable
isotopic trends in amphibolite to granulite facies transitions metamorphic
or diagenetic ? - An answer for the Arendal area (Bamble sector, SE Norway)
from Mid-Proterozoic carbon-bearing rocks. Amer. J. Sci. 294:1135-1165.

Clemens, J.D., 1993. Experimental evidence against CO2-promoted deep
crustal melting. Nature 363:336-338.

Farquhar, J. & Chacko, T., 1991. Isotopic evidence for involvement of
CO2-bearing magmas in granulite formation. Nature 354:60-63. 

Gibert, F., Guillaume, D. & Laporte, D., 1998. Importance of fluid
immiscibility in the H2O-NaCl-CO2 system and selective CO2 entrapment in
granulites: Experimental phase diagram at 5-7 kbar, 900°C and wetting
textures. Eur. J. Mineral. 10:1109-1123.

Giorgetti, G., Frezzotti, M.L., Carosi, R., Meccheri, M. & Touret, J.L.R.,
1997. Carbonic fluid evolution in syntectonic veins in metapelites and
marbles from Priestley formation (Northern Victoria Land, Antarctica). In:
Ricci, C.A., ed., The Antarctic region; geological evolution and processes.
Proceedings of the 7th International Symposium on Antarctic Earth Sciences.
Cambridge Univ. Press, Cambridge, 279-282. 

Glassley, W.E., 1982. Fluid evolution and graphite genesis in the deep
continental crust. Nature 295:229-231

Glassley, W.E., 1983. The role of CO2 in the chemical modification of deep
continental crust. Geoch. Cosm. Acta 47:597-616. 

Glassley, W.E., Ryerson, F.J., Shaw, H. & Abeysinghe, P.B., 1989. Chemical
changes associated with formation of granulite and migration of complex
C-O-H-S fluids, Sri Lanka. In: Bridgwater, D., ed., Fluid movements -
element transport and the composition of the deep crust. Kluwer, Dordrecht,
39-49. 

Graphchikov, A.A., Konilov, A.N. & Clemens, J.D., 1999. Biotite
dehydration, partial melting, and fluid composition: Experiments in the
system KAlO2 - FeO - MgO - SiO2 - H2O - CO2. Amer. Mineral. 84:15-26. 

Harley, S.L. & Santosh, M., 1995. Wollastonite at Nuliyam, Kerala, southern
India: A reassessment of CO2-infiltration and charnockite formation at a
classic locality. Contr. Mineral. Petrol. 120:83-94.

Harris, N.B.W., Jackson, D.H., Mattey, D.P., Santosh, M. & Bartlett, J.,
1993. Carbon-isotope constraints on fluid advection during contrasting
examples of incipient charnockite formation. J. Metam. Geol. 11:833-846.

Hoefs, J., Coolen, J.J.M. & Touret, J., 1981. The sulfur and carbon isotope
composition of scapolite-rich granulites from southern Tanzania. Contr.
Mineral. Petrol. 78:332-336. 

Johnson, E.L., 1991. Experimentally determined limits for H2O - CO2 - NaCl
immiscibility in granulites. Geology 19:925-928.

Kaszuba, J.P. & Wendlandt, R.F., 2000. Effect of carbon dioxide on
dehydrtion melting reactions and melt compositions in the lower crust and
the origin of alkaline rocks. J. Petrol. 41:363?386.

Lamb, W.M. & Moecher, D.P., 1992. CO2-rich fluid inclusions in the
Whitestone anorthosite: Implications for the retrograde history of the
Parry Sound shear zone, Grenville province, Canada. J. Metam. Geol. 10:763-776

Lamb, W. & Valley, J.W., 1984. Metamorphism of reduced granulites in
low-CO2 vapour-free environment. Nature 312:56-58. 

Lamb, W.M. & Valley, J.W., 1985. C-O-H fluid calculations and granulite
genesis. In: Tobi, A.C. & Touret, J.L.R., eds., The deep Proterozoic crust
in the North Atlantic provinces. D. Reidel, Dordrecht, 119-131.

Litvinovskiy, B.A., 1995. H2O - CO2 fluids in the lower and middle crust:
Their role in magma formation and  metamorphism. Dokl. Ross. Ak. Nauk
333:80-84

Moecher, D.P., 1993. Scapolite phase equilibria and carbon isotopes ?
Constraints on the nature and distribution of CO2 in the lower continental
crust. Chem. Geol. 108:163?174.

Moecher, D.P. & Essene, E.J., 1990. Scapolite phase equilibria: Additional
constraints on the role of CO2 in granulite genesis. In: Vielzeuf, D. &
Vidal, P., eds., Granulites and crustal evolution. Kluwer, Dordrecht, 385-396.

Moecher, D.P. & Essene, E.J., 1990. Phase equilibria for calcic scapolite
and implications for variable Al-Si disorder for P-T, T-XCO2 and a-X
relations, J. Petrol. 31:997-1024.

Moecher, D.P. & Essene, E.J., 1992. Calculation of CO2 activities using
scapolite phase equilibria: Constraints on the presence and composition of
a fluid phase during high-grade metamorphism. Contr. Mineral. Petrol.
108:219-240.

Newton, R.C., 1989. Metamorphic fluids in the deep crust. Ann. Rev. Earth
Plan. Sci. 17:385-412

Newton, R.C., 1990. Fluids and shear zones in the deep crust. Tectonoph.
182:21-37. 

Newton, R.C., 1992. Charnockitic alteration: Evidence for CO2 infiltration
in granulite facies metamorphism. J. Metam. Geol. 10:383-400. 

Newton, R.C. & Manning, C.E., 2000. Quartz solubility in the H2O - NaCl and
H2O - CO2 solutions at deep crust- upper mantle pressures and temperatures:
2 - 15 kbar and 500 - 900°C. Geochim. Cosmochim. Acta 64:2993-3005.

Newton, R.C., Smith, J.V. & Windley, B.F., 1980. Carbonic metamorphism,
granulites and crustal growth. Nature 288:45-50. 

Perchuk, L.L. & Gerya, T.V., 1992. The fluid regime of metamorphism and the
charnockite reaction in granulites: A review. Int. Geol. Rev. 34:1-58.

Perchuk, L.L. & Gerya, T.V., 1993. Fluid control of charnockitization.
Chem. Geol. 108:175?186.

Peterson, J.W. & Newton, R.C., 1989. CO2-enhanced melting of
biotite-bearing rocks at deep-crustal pressure - temperature conditions.
Nature 340:378-380.

Peterson, J.W. & Newton, R.C., 1990. Experimental biotite-quartz melting in
the KMASH-CO2 system and the role of CO2 in the petrogenesis of granites
and related rocks. Amer. Mineral. 75:1029-1042.

Rumble III, D., Chamberlain, C.P., Zeitler, P.K. & Barreiro, B., 1989.
Hydrothermal graphite veins and Acadian granulite metamorphism, New
Hampshire, USA. In: Bridgwater, D., ed., Fluid movements - element
transport and the composition of the deep crust. Kluwer, Dordrecht, 117-119.

Santosh, M., 1992. Carbonic fluids in granulites: Cause or consequence ? J.
Geol. Soc. India 39:375-399. 

Santosh, M., Jackson, D.H. & Harris, N.B.W., 1993. The significance of
channel and fluid-inclusion CO2 in cordierite: Evidence from carbon
isotopes. J. Petrol. 34:233-258.

Santosh, M., Jackson, D.H., Harris, N.B.W. & Mattey, D.P., 1991. Carbonic
fluid inclusions in south Indian granulites: Evidence for entrapment during
charnockite formation. Contr. Mineral. Petrol. 108:318-330. 

Santosh, M. & Wada, H., 1993. Microscale isotopic zonation in graphite
crystals ? Evidence for channelled CO2 influx in granulites. EPSL 119:19?26. 

Santosh, M. & Wada, H., 1993. A carbon isotope study of graphites from the
Kerala khondalite belt, southern India: Evidence for CO2 infiltration in
granulites. J. Geol. 101:643-651.

Satish-Kumar, M. & Santosh, M., 1998. A petrological and fluid inclusion
study of calc-silicate-charnockite associations from southern Kerala,
India: Implications for CO2 influx. Geol. Mag. 135:27-45

Schalkwyk, J.F. van & Reenen, D.D. van, 1992. High-temperature hydration of
ultramafic granulites from the Southern marginal zone of the Limpopo belt
by infiltration of CO2-rich fluid. Precamb. Res. 55:337-352

Schuiling, R.D. & Kreulen, R., 1979. Are thermal domes heated by CO2-rich
fluids from the mantle. EPSL 43:298-302.

Srikantappa, C., Raith, M. & Touret, J.L.R., 1992. Synmetamorphic
high-density carbonic fluids in the lower crust: Evidence from the Nilgiri
granulites, southern India. J. Petrol. 33:733-760.

Srikantappa, C. & Valley, J.W., 1992. Oxygen and carbon isotopic
composition of Precambrian carbonates from Karnataka and Tamilnadu, India.
J. Geol. Soc. India 40:341?346

Stevens, G., 1997. Melting, carbonic fluids and water recycling in thee
deep crust: An example from the Limpopo belt, South Aftica. J. Metam. Geol.
15:141-154.

Touret, J.L.R., 1970. Le faciès granulite, métamorphisme en milieu
carbonique. C. R. Ac. Sci. Paris 271D:2228-2231.

Touret, J.L.R., 1971. Le faciès granulite en Norvège méridionale. II Les
inclusions fluides. Lithos 4:423-436.

Touret, J.L.R., 1971. Controle du faciès granulite dans le Bamble par le
CO2 de la phase fluide. C. R. Sommaire  Soc. Fr. Géol. 3:143-146.

Touret, J.L.R., 1974. Faciès granulite et fluides carboniques. In:
Bellière, J. & Duchesne, J.C., eds., Géologie des domaines cristallins.
Soc. Belg. Géol., Liège, 267-287.

Touret, J.L.R., 1985. Fluid regime in southern Norway: the record of fluid
inclusions. In: Tobi, A.C. & Touret, J.L.R., eds., The deep Proterozoic
crust in the North Atlantic provinces. D. Reidel, Dordrecht, 517-549.

Touret, J.L.R., 1986. Fluid inclusions in rocks from the lower continental
crust. In: Dawson, J.B., Carswell, D.A., Hall, J. & Wedepohl, K.H., eds.,
The nature of the lower continental crust. Geol. Soc. Spec. Publ. 24:161-172. 

Touret, J.L.R., 1995. The role and nature of fluids in the continental
lower crust. In: Yoshida, M. & Santosh, N., eds., India and Antarctica
during the Precambrian. Geol. Soc. India Mem. 34:143-160.

Touret, J.L.R. & Hartel, T.H.D., 1990. Synmetamorphic fluid inclusions in
granulites. In: Vielzeuf, D. & Vidal, P., eds., Granulites and crustal
evolution. D. Reidel, Dordrecht, 397-417.

Valley, J.W., Bohlen, S.R., Essene, E.J. & Lamb, W., 1990. Metamorphism in
the Adirondacks: II. The role of fluids. J. Petrol. 31:555-596.

Valley, J.W., McLelland, J., Essene, E.J. & Lamb, W.M., 1983. Metamorphic
fluids in the deep crust: Evidence from the Adirondacks. Nature 301:226-228. 

Vry, J.K., Brown, P.E. & Valley, J.W., 1990. Cordierite volatile content
and the role of CO2 in high-grade metamorphism. Amer. Mineral. 75:71-88.

Wendlandt, R.F., 1981. Influence of CO2 on melting of model granulite
facies assemblages: A model for the genesis of charnockites. Amer. Mineral.
66:1164-1174.

Yardley, B.W.D. & Valley, J.W., 1997. The petrologic case for a dry lower
crust. J. Geophys. Res. 102B:12173-12185.

Valley, J.W. & O'Neil, J.R., 1984. Fluid heterogeneity during granulite
facies metamorphism in the Adirondacks: Stable isotope evidence. Contr.
Mineral. Petrol. 85:158-173. 


At 15:05 30-10-2002 +0100, you wrote:
>Dear all,
>I would appreciate it very much if you could send me any references
>about the role of CO2, and models for its genesis/occurrence, in
>granulites.
>I already searched in Georef and WoS, but I wouldn't want to miss
>important contributions.
>
>Thank you very much for your help,
>B. Cesare
>--
>
>******************************************************
>Bernardo Cesare
>Dipartimento di Mineralogia e Petrologia, Universita' di Padova
>Corso Garibaldi, 37, I-35137 PADOVA     ITALY
>Tel: ++39-49-8272019    Fax: ++39-49-8272010
>[log in to unmask]
>http://dmp.unipd.it/bernardo/bernardo.html
>******************************************************
>
>

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