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Definition, Conditions and Types of Metamorphism

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Petrogenesis of Metamorphic Rocks

Abstract

The process of rock metamorphism changes the mineralogical and chemical composition, as well as the structure of rocks. Metamorphism is typically associated with elevated temperature and pressure; thus it affects rocks within the earth’s crust and mantle. The process is driven by changing physical and/ or chemical conditions in response to large-scale geological dynamics. Consequently, it is inherent in the term, that metamorphism is always related to a precursor state where the rocks had other mineralogical and structural attributes. Metamorphism, metamorphic processes and mineral transformations in rocks at elevated temperatures and pressures are fundamentally associated with chemical reactions in rocks. Metamorphism does not include, by definition, similar processes that occur near the earth’s surface such as weathering, cementation and diagenesis. The transition to igneous processes is gradual; metamorphism may include partial melting. The term metasomatism is used if modification of the bulk composition of rocks is the dominant metamorphic process. Metamorphic rocks are rocks that developed their mineralogical and structural characteristics by metamorphic processes.

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References

  • Alt JC (1999) Very low-grade hydrothermal metamorphism of basic igneous rocks. In: Frey

    Google Scholar 

  • M, Robinson D (eds) Low-grade metamorphism. Blackwell, Oxford, pp 169–201

    Google Scholar 

  • Bevins RE, Robinson D (1988) Low grade metamorphism of the Welsh Basin Lower Paleozoic succession: an example of diastathermal metamorphism? J Geol Soc Lond 145: 363–366

    Article  Google Scholar 

  • Bischoff A, Stöffler D (1992) Shock metamorphism as a fundamental process in the evolu- tion of planetary bodies: information from meteorites. Eur J Mineral 4: 707–755

    Google Scholar 

  • Boles JR, Coombs DS (1975) Mineral reactions in zeolitic Triassic tuff, Hokonui Hills, New Zealand. Geol Soc Am Bull 86: 163–173

    Google Scholar 

  • Buick IS, Cartwright I (1996) Fluid-rock interaction during low-pressure polymetamor-phism of the Reynolds Range Group, central Australia. J Petrol 37: 1097–1124

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Coleman RG, Wang X (eds) (1995) Ultrahigh pressure metamorphism. Cambridge Univer-sity Press, Cambridge, 528 pp

    Chapter  Google Scholar 

  • Cooke RA, O’Brien PJ, Carswell DA (2000) Garnet zoning and the identification of equilib-rium mineral compositions in high-pressure-temperature granulites from the Moldanu-bian Zone, Austria. J Metamorph Geol 18: 551–569

    Google Scholar 

  • Coombs DS (1961) Some recent work on the lower grades of metamorphism. Aust J Sci 24: 203–215

    Google Scholar 

  • Dempster TJ, Bluck BJ (1995) Regional metamorphism in transform zones during supercon-tinent breakup: late Proterozoic events of the Scottish Highlands. Geology 23:991–994 Dietz RS (1961) Astroblemes. Sci Am 205: 50–58

    Google Scholar 

  • Droop GTR, Al-Filali IY (1996) Interaction of aqueous fluids with calcareous metasediments during high-T, low-P regional metamorphism in the Qadda area, southern Arabian Shield. J Metamorph Geol 14: 613–634

    Article  Google Scholar 

  • Ellis DJ (1980) Osumilite-sapphirine-quartz-granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolu-tion of the deep crust. Contrib Mineral Petrol 74: 201–210

    Article  Google Scholar 

  • Emmermann R, Lauterjung J (1997) The German Continental Deep Drilling Program KTB. J Geophys Res 102: 18179–18201

    Article  Google Scholar 

  • Ernst WG (1999) Metamorphism, partial preservation, and exhumation of ultrahigh-pres-sure belts. Island Arc 8: 125–153

    Article  Google Scholar 

  • Frey M, Kisch HJ (1987) Scope of subject. In: Frey M (ed) Low temperature metamorphism. Blackie, Glasgow, pp 1–8

    Google Scholar 

  • Gianelli G, Grassi S (2001) Water-rock interaction in the active geothermal system of Pan-telleria, Italy. Chem Geol 181: 113–130

    Google Scholar 

  • Giggenbach WF (1981) Geothermal mineral equilibria. Geochim Cosmochim Acta 45: 393–410

    Article  Google Scholar 

  • Giggenbach WF (1984) Mass transfer in hydrothermal alteration systems–a conceptual ap-proach. Geochim Cosmochim Acta 48: 2693–2711

    Article  Google Scholar 

  • Gillis KM (1995) Controls on hydrothermal alteration in a section of fast-spreading oceanic crust. Earth Planet Sci Lett 134: 473–489

    Article  Google Scholar 

  • Grieve RAF (1987) Terrestrial impact structures. Annu Rev Earth Planet Sci 15: 245–270

    Article  Google Scholar 

  • Hacker BR, Ratschbacher L, Webb L, Shuwen D (1995) What brought them up? Exhumation of the Dabie Shan ultrahigh-pressure rocks. Geology 23: 743–746

    Article  Google Scholar 

  • Harley SL, Motoyoshi Y (2000) Al zoning in orthopyroxene in a sapphirine quartzite: evi-dence for 1120°C UHT metamorphism in the Napier Complex, Antarctica, and implica-tions for the entropy of sapphirine. Contrib Mineral Petrol 138: 293–307

    Google Scholar 

  • Hokada T (2001) Feldspar thermometry in ultrahigh-temperature metamorphic rocks: evi-dence of crustal metamorphism attaining,-z1100’C in the archean Napier Complex, East Antarctica. Am Mineral 86: 932–938

    Google Scholar 

  • Holmes A (1920) The nomenclature of petrology, 1st edn. Murby, London, 284 pp

    Google Scholar 

  • Kawachi DE (1975) Pumpellyite-actinolite and contiguous facies metamorphism in the

    Google Scholar 

  • Upper Wakatipu district, southern New Zealand. N Z J Geol Geophys 17:169–208

    Google Scholar 

  • Kerrick DM (ed) (1991) Contact metamorphism. Reviews in mineralogy, vol 26. Mineralogi-cal Society of America, Washington, DC, 847 pp

    Google Scholar 

  • Kienast JR, Lombardo B, Biino G, Pinardon JL (1991) Petrology of very-high-pressure eclo-gitic rocks from the Brossacasco-Isasca Complex, Dora-Maira Massif, Italian Western Alps. J Metamorph Geol 9: 19–34

    Google Scholar 

  • Kisch HJ (1987) Correlation between indicators of very-low-grade metamorphism. In: Frey M (ed) Low temperature metamorphism. Blackie, Glasgow, pp 227–300

    Google Scholar 

  • Kozlovsky YA (1984) The world’s deepest well. Sci Am 251: 106–112

    Article  Google Scholar 

  • Lamb RC, Smalley PC, Field D (1986) P-T conditions for the Arendal granulites, southern Norway: implications for the roles of P, T and CO2 in deep crustal LILE-depletion. J Metamorph Geol 4: 143–160

    Article  Google Scholar 

  • Levi B, Aguirre L, Nystroem JO (1982) Metamorphic gradients in burial metamorphosed vesicular lavas; comparison of basalt and spilite in Cretaceous basic flows from central Chile. Contrib Mineral Petrol 80: 49–58

    Article  Google Scholar 

  • Merriman RJ, Frey M (1999) Patterns of very low-grade metamorphism in metapelitic rocks. In: Frey M, Robinson D (eds) Low-grade metamorphism. Blackwell, Oxford, pp 61–107

    Google Scholar 

  • Miyashiro A (1972) Pressure and temperature conditions and tectonic significance of regional and ocean floor metamorphism. Tectonophysics 13: 141–159

    Article  Google Scholar 

  • Miyashiro A (1973) Metamorphism and metamorphic belts. Allen and Unwin, London, 492 pp

    Book  Google Scholar 

  • Miyashiro A, Shido F, Ewing M (1971) Metamorphism in the mid-Atlantic ridge near 24° and 30°N. Philos Trans R Soc Lond A268: 589–603

    Article  Google Scholar 

  • Möller P, Weise SM, Althaus E, Bach W, Behr HJ, Borchardt R, Bräuer K, Drescher F, Erzinger J, Faber E, Hansen BT, Horn EE, Huenges E, Kämpf H, Kessels N, Kirsten T, Landwehr D, Lodemann M, Machon L, Pekdeger A, Pielow H-U, Reutel C, Simon K, Walther J, Weinlich FH, Zimmer M (1997) Paleo-and recent fluids in the upper continental crust - results from the German Continental deep drilling Program ( KTB ). J Geophys Res 102: 18245–18256

    Google Scholar 

  • Newton RC (1987) Petrologic aspects of Precambrian granulite facies terrains bearing on their origins. In: Kröner A (ed) Proterozoic Lithospheric evolution. Am Geophys Union Geodyn Ser 17: 11–26

    Google Scholar 

  • Okay AI (1993) Petrology of a diamond-and coesite-bearing metamorphic terrain: Dabie Shan, China. Eur J Mineral 5: 659–675

    Google Scholar 

  • Reinecke T (1991) Very-high-pressure metamorphism and uplift of coesite-bearing meta-sediments from the Zermatt-Saas zone, Western Alps. Eur J Mineral 3: 7–17

    Google Scholar 

  • Robinson D (1987) Transition from diagenesis to metamorphism in extensional and colli-sion settings. Geology 15: 866–869

    Article  Google Scholar 

  • Robinson D, Merriman RJ (1999) Low-temperature metamorphism: an overview. In: Frey M, Robinson D (eds) Low-grade metamorphism. Blackwell, Oxford, pp 1–9

    Google Scholar 

  • Robinson D, Bevins RE (1999) Patterns of regional low-grade metamorphism in metabasites. In: Frey M, Robinson D (eds) Low-grade metamorphism. Blackwell, Oxford, pp 143–168

    Google Scholar 

  • Schertl HP, 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 PT-path. Contrib Mineral Petrol 108: 1–21

    Article  Google Scholar 

  • Schreyer W (1995) Ultradeep metamorphic rocks: the retrospective viewpoint. J Geophys Res 100: 8353–8366

    Article  Google Scholar 

  • Seki Y (1973) Temperature and pressure scale of low-grade metamorphism. J Geol Soc Jpn 79: 735–743

    Article  Google Scholar 

  • Shatsky VS, Sobolev NV, Vavilow MA (1995) Diamond-bearing metamorphic rocks of the Kokchetav massif (northern Kazakhstan). In: Coleman RG, Wang X (eds) Ultrahigh pressure metamorphism. Cambridge University Press, Cambridge, pp 427–455

    Chapter  Google Scholar 

  • Smith DC, Lappin MA (1989) Coesite in the Straumen kyanite-eclogite pod, Norway. Terra Nova 1: 47–56

    Google Scholar 

  • Smith RE (1969) Zones of progressive regional burial metamorphism in part of the Tasman geosyncline, eastern Australia. J Petrol 10: 144–163

    Article  Google Scholar 

  • Stern CR, Wyllie PJ (1981) Phase relationships of I-type granite with H2O to 35 kilobars: the Dinkey Lakes biotite-granite from the Sierra Nevada batholith. J Geophys Res 86 (B11): 10412–10422

    Article  Google Scholar 

  • Teichmüller M (1987) Organic material and very low-grade metamorphism. In: Frey M (ed) Low temperature metamorphism. Blackie, Glasgow, pp 114–161

    Google Scholar 

  • Vernon RH (1976) Metamorphic processes. Allen and Unwin, London, 247 pp

    Google Scholar 

  • Wain A, Waters D, Jephcoat A, Olijynk H (2000) The high-pressure to ultrahigh-pressure eclogite transition in the Western Gneiss Region, Norway. Eur J Mineral 12: 667–688

    Google Scholar 

  • Winkler HGF (1974, 1976, 1979 ) Petrogenesis of metamorphic rocks, 3rd, 4th, and 5th edn. Springer, Berlin Heidelberg New York

    Chapter  Google Scholar 

  • Wise DU, Dunn DE, Engelder JT, Geiser PA, Hatcher RD, Kish SA, Odon AL, Schamel S (1984) Fault-related rocks: suggestions for terminology. Geology 12: 391–394

    Article  Google Scholar 

  • Yang J, Godard G, Kienast JR, Lu Y, Sun J (1993) Ultrahigh-pressure (60 kbar) magnesite-bearing garnet peridotites from northeastern Jiangsu, China. J Geol 101: 541–554

    Google Scholar 

  • Zhang R-Y, Liou JG (1994) Coesite-bearing eclogite in Henan Province, central China: detailed petrography, glaucophane stability and PT-path. Eur J Mineral 6: 217–233

    Google Scholar 

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Authors and Affiliations

  1. Institute of Mineralogy, Petrology and Geochemistry, University of Freiburg, Albertstr. 23b, 79104, Freiburg i. Br., Germany

    Professor Dr. Kurt Bucher

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  1. Professor Dr. Kurt Bucher
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  2. Professor Dr. Martin Frey
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Bucher, K., Frey, M. (2002). Definition, Conditions and Types of Metamorphism. In: Petrogenesis of Metamorphic Rocks. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-04914-3_1

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  • DOI: https://doi.org/10.1007/978-3-662-04914-3_1

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-662-04916-7

  • Online ISBN: 978-3-662-04914-3

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