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Metamorphe Mineralfazies

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Mineralogie

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Zusammenfassung

Durch prograde Mineralreaktionen entstehen in metamorphen Gesteinen – je nach ihrer chemischen Zusammensetzung – charakteristische Mineralparagenesen. Diese repräsentieren beim Höhepunkt der Metamorphose zumindestens angenähert ein thermodynamisches Gleichgewicht und spiegeln dementsprechend die erreichten Drücke und Temperaturen wider. Die Gesamtheit aller Paragenesen, die in metamorphen Gesteinen mit unterschiedlichem Chemismus, aber bei etwa gleichen P-T-Bedingungen gebildet wurden, definieren eine metamorphe Fazies.

†Deceased

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Weiterführende Literatur

(Siehe auch Kap. 24 und 25)

  • Best, MG (2003) Igneous and metamorphic petrology, 2nd edn. Freeman, San Francisco

    Google Scholar 

  • Bucher K, Frey M (2002) Petrogenesis of metamorphic rocks, 7th edn. Springer, Berlin Heidelberg New York

    Google Scholar 

  • Ernst WG (1976) Petrologic phase equilibria. Freeman, San Francisco

    Google Scholar 

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

    Google Scholar 

  • Miyashiro A (1994) Metamorphic petrology. UCL Press, London

    Google Scholar 

  • Spear FS (1993) Metamorphic phase equilibria and pressure– temperature–time paths.Mineral SocAmerica,Washington, DC

    Google Scholar 

  • Yardley BWD (1989) An introduction to metamorphic petrology. Longman, Burnt Mill, Harlow, Essex, England

    Google Scholar 

Zitierte Literatur

  • Bearth P (1973) Gesteins- und Mineralparagenesen aus den Ophiolithen von Zermatt. Schweiz Mineral Petrogr Mitt 53:299–334

    Google Scholar 

  • Becke F (1903) Über Mineralbestand und Struktur der Kristallinen Schiefer. Denkschr Akad Wiss Wien 75:97 ff

    Google Scholar 

  • Brandt S, Will TM, Klemd R (2007) Magmatic loading in the proterozoic Epupa Complex, NW Nambia, as evidenced by ultrahigh-temperature sapphirine-bearing orthopyroxene-sillimanitequartz granulites. Prec Research 153:143–178

    Article  Google Scholar 

  • Carlson WD, Rosenfeld JL (1981) Optical determination of topotactic aragonite-calcite growth kinetics: Metamorphic implications. J Geol 89:615–638

    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 

  • Chopin C (2003) Ultrahigh-pressure metamorphism: Tracing continental crust into the mantle. Earth Planet Sci Lett 212:1–14

    Article  Google Scholar 

  • Compagnoni R, Maffeo B (1973) Jadeite-bearing metagranites l. s. and related rocks in the Mount Mucrone area (Sesia-Lanzo Zone, Western Italian Alps). Schweiz Mineral Petrogr Mitt 53:355–378

    Google Scholar 

  • Coombs DS (1960) Lower grade mineral facies in New Zealand. Internat Geol Congr 21st Sess Rep Part 13:339–351, Copenhagen

    Google Scholar 

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

    Google Scholar 

  • Eskola P (1915) On the relations between the chemical and mineralogical composition in the metamorphic rocks of the Orijärvi region. Bull Comm géol Finlande 44 (English summary p 109–145)

    Google Scholar 

  • Eskola P (1939) Die metamorphen Gesteine. In: Barth TF, Correns CW, Eskola P (1970) Die Entstehung der Gesteine – Ein Lehrbuch der Petrogenese, 3. Teil. Springer, Berlin, S 263–407 (Neudruck)

    Google Scholar 

  • Evans BW (1990) Phase relations of epidote-blueschists. Lithos 25:3–23

    Article  Google Scholar 

  • Goldschmidt VM (1911) Die Kontaktmetamorphose im Kristianiagebiet. Oslo Vidensk Skr, I Math-Nat Kl, no 11

    Google Scholar 

  • Grubenmann U (1904, 1910) Die kristallinen Schiefer, 1. und 2. Aufl. Borntraeger, Berlin

    Google Scholar 

  • Grubenmann U, Niggli P (1924) Die Gesteinsmetamorphose. I: Allgemeiner Teil. Borntraeger, Berlin

    Google Scholar 

  • Harley SL (1998) On the occurrence and characterization of ultrahigh-temperature crustal metamorphism. In: Treloar PJ, O’Brien PJ (eds) What drives metamorphism and metamorphic reactions? Geol Soc London, Spec Publ 138:81–107

    Google Scholar 

  • Heinrich W, Althaus E (1988) Experimental determination of the reactions 4 Lawsonite + 1 Albite = 1 Paragonite + 2 Zoisite + 2 Quartz + 6 H2O and 4 Lawsonite + 1 Jadeite = 1 Paragonite + 2 Zoisite + 1 Quartz + 6 H2O. Neues Jahrb Mineral Monatsh 1988:516–528

    Google Scholar 

  • Holdaway MJ (1971) Stability of andalusite and the aluminum silicate phase diagram. Amer J Sci 271:97–131

    Google Scholar 

  • Holland TJB (1979) Experimental determination of the reaction paragonite = jadeite + kyanite + H2O, and internally consistent thermodynamic data for part of the system Na2O–Al2O3–SiO2–H2O, with applications to eclogites and blueschists. ContribMineral Petrol 68:293–301

    Article  Google Scholar 

  • Kulke H, Schreyer W (1973) Kyanite-talc schist from Sar e Sang, Afghanistan. Earth Planet Sci Lett 18:324–328

    Article  Google Scholar 

  • Liou JG, Kim HS, Maruyama S (1983) Prehnite–epidote equilibria and their petrologic applications. J Petrol 24:321–342

    Google Scholar 

  • Maresch WV (1977) Experimental studies on glaucophane: An analysis of present knowledge. Tectonophysics 43:109–125

    Article  Google Scholar 

  • Miyashiro A (1961) Evolution of metamorphic belts. J Petrol 2:277–311

    Google Scholar 

  • Nasdala L, Massonne H-J (2000) Microdiamonds from the Saxonian Erzgebirge, Germany: In-situ micro-Raman characterisation. Eur J Mineral 12:495–498

    Google Scholar 

  • O’Brien PJ (1993) Partially retrograded eclogites of the Münchberg Massif, Germany: Records of a multistage Variscan uplift history in the Bohemian Massif. J Metamorph Geol 11:241–260

    Article  Google Scholar 

  • O’Brien PJ (2006) Type-locality granulites: high-pressure rocks formed at eclogite-facies conditions. Mineral Petrol 86:161–175

    Article  Google Scholar 

  • Okrusch M, Matthes S, Klemd R, O’Brien PJ, Schmidt K (1991) Eclogites at the northwestern margin of the Bohemian Massif: A review. Eur J Mineral 3:707–730

    Google Scholar 

  • Robinson P, Spear FS, Schumacher JC, Laird J, Klein C, Evans BW, Doolan BL (1982) Phase relations in metamorphic amphiboles: Natural occurrence and theory. In: Veblen DR, Ribbe PH (eds) Amphiboles: Petrology and experimental phase relations. Rev Mineral 9B:1–227

    Google Scholar 

  • Schiffman P, Liou JG (1980) Synthesis and stability relations of Mg-Al pumpellyite, Ca4Al5MgSi6O21(OH)7. J Petrol 21:441–474

    Google Scholar 

  • Schliestedt M (1986) Eclogite-blueschist relationships as evidenced by mineral equilibria in the high-pressure metabasic rocks of Sifnos (Cycladic Islands), Greece. J Petrol 27:1437–1459

    Google Scholar 

  • Schliestedt M, Okrusch M (1988) Meta-acidites and silicic metasediments related to eclogites and glaucophanites in northern Sifnos, Cycladic Archipelago, Greece.In: Smith DC (ed) Eclogites and eclogite-facies rocks, 291–334. Elsevier, Amsterdam

    Google Scholar 

  • Schmädicke E (1994) Die Eklogite des Erzgebirges. Freiberger Forschunghefte C456, 338 pp. Verlag für Grundstoffindustrie, Leipzig Stuttgart

    Google Scholar 

  • Schmädicke E, Will TM (2003) Pressure–temperature evolution of blueschist facies rocks from Sifnos, Greece, and implications for the exhumation of high-pressure rocks in the Central Aegean. J Metam Geol 21:799–811

    Article  Google Scholar 

  • Schmidt MW, Poli S (1994) 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 Sci Lett 124:105–118

    Article  Google Scholar 

  • Schreyer W (1974) Whiteschist: A new type of metamorphic rock formed at high pressures. Geol Rundschau 63:597–609

    Article  Google Scholar 

  • Schreyer W (1988) Experimental studies on metamorphism of crustal rocks under mantle pressures. Mineral Mag 52:1–26

    Article  Google Scholar 

  • Theye T, Seidel E (1991) Petrology of low-grade high-pressure metapelites from the External Hellenides (Crete, Peloponnese) – A case study with attention of sodic minerals. Eur J Mineral 3:343–366

    Google Scholar 

  • Theye T, Seidel E,Vidal O (1992) Carpholite, sudoite, and chloritoid in low-grade high-pressure metapelites from Crete and the Peloponnese, Greece. Eur J Mineral 4:487–507

    Google Scholar 

  • Thompson JB Jr (1957) The graphical analysis of mineral assemblages in pelitic schists. Am Mineral 42:842–858

    Google Scholar 

  • Turner FJ,Verhoogen J (1960) Igneous and metamorphic petrology. 2nd ed, McGraw-Hill, New York

    Google Scholar 

  • Turner FJ (1981) Metamorphic petrology. Mineralogical, field, and tectonic aspects, 2nd edn. McGraw-Hill, New York

    Google Scholar 

  • Will T, Okrusch M, Schmädicke E, Chen G (1998) Phase relations in the greenschist-blueschist-amphibolite-eclogite facies in the system Na2O–CaO–FeO–MgO–Al2O3–SiO2–H2O, with application to metamorphic rocks from Samos, Greece. Contrib Mineral Petrol 132:85–102

    Article  Google Scholar 

  • Williams GW (1890) The greenstone schist areas of the Menominee and Marquette regions of Michigan. US Geol Surv Bull no 62 Winkler HGF (1965, 1967) Die Genese der metamorphen Gesteine, 1. und 2. Aufl. Springer,

    Google Scholar 

  • Winkler HGF (1979) Petrogenesis of metamorphic rocks, 5th edn. Springer, New York Heidelberg Berlin

    Google Scholar 

  • Yoder HS, Tilley CE (1962) Origin of basalt magmas: An experimental study of natural and synthetic rock systems. J Petrol 3:342–532

    Google Scholar 

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Authors and Affiliations

  1. Lehrstuhl für Geodynamik und Geomaterialforschung Universität Würzburg, Am Hubland, 97074, Würzburg, Germany

    Dr. Martin Okrusch (Professor)

Authors
  1. Dr. Martin Okrusch
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  2. Dr. Siegfried Matthes †
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Okrusch, M., Matthes †, S. (2010). Metamorphe Mineralfazies. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_26

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