Tham khảo Biến chất nhiệt độ siêu cao

  1. ↑ S.L., Harley (1998). “On the occurrence and characterization of ultrahigh-temperature crustal metamorphism” 138. tr. 81–107. doi:10.1144/GSL.SP.1996.138.01.06. 
  2. 1 2 Brown, M. (2007). “Metamorphic conditions in orogenic belts: a record of secular change”. International Geology Review 49: 193-234. Truy cập ngày 6 tháng 10 năm 2010.  Đã bỏ qua tham số không rõ |vol= (trợ giúp)
  3. 1 2 Kelsey, D.E., 2008, On ultra-high temperature crustal metamorphism. Gondwana Research 13, 1-29
  4. 1 2 Santosh, M.; Omori, S. (2008). “CO2 flushing: a plate tectonic perspective”. Gondwana Research 13: 86-102. Truy cập ngày 6 tháng 10 năm 2010.  Đã bỏ qua tham số không rõ |vol= (trợ giúp); Chú thích sử dụng tham số |coauthor= bị phản đối (trợ giúp)
  5. 1 2 Omori, S. (2008). “CO2 windows from mantle to atmosphere: Models on ultrahigh- temperature metamorphism and speculations on the link with melting of snowball Earth”. Gondwana Research 14. doi:10.1016/j.gr.2007.11.001. Truy cập ngày 6 tháng 10 năm 2010.  Đã bỏ qua tham số không rõ |vol= (trợ giúp)
  6. ↑ Arima, M., and Barnett, R. L., 1984, Sapphirine bearing granulites from the Sipiwesk Lake area of the late Archean Pikwitonei granulite terrain, Manitoba, Canada: Contributions to Mineralogy and Petrology, v. 88, p. 102-112.
  7. ↑ Harley, S. L., 1985, Garnet-orthopyroxene bearing granulites from Enderby Land, Antarctica: Metamorphic pressure-temperature-time evolution of the Archaean Napier Complex: Journal of Petrology, v. 26, p. 819-856.
  8. ↑ Harley, S. L., and Motoyoshi, Y., 2000, Al zoning in orthopyroxene in a sapphirine quartzite: Evidence for >1120°C UHT metamorphism in the Napier complex, Antarctica, and implications for the entropy of sapphirine: Contributions to Mineralogy and Petrology, v.138, p. 293–307.
  9. ↑ Fonarev, V. I., Pilugin, S. M., Savko, K. A., and Novikova, M. A., 2006, Exsolution textures of ortho-and clinopyroxene in high-grade BIF of the Voronezh Crystalline Massif: Evidence of ultrahigh-temperature metamorphism: Journal of Metamorphic Geology, v. 24, p. 135-151.
  10. ↑ Tsunogae et al., 2002
  11. 1 2 Santosh, M. Sajeev K. and J. Li 2006, Extreme crustal metamorphism during Columbia supercontinent assembly: Evidence from North China Craton. Gondwana Research, v. 10, p. 256-266.
  12. 1 2 Santosh, M., Tsunogae, T., Li, J.H., and Liu, S.J., 2007, Discovery of sapphirine- bearing Mg-Al granulites in the North China Craton: Implications for Paleoproterozoic ultrahigh- temperature metamorphism. Gondwana Research 11, 263-285.
  13. 1 2 3 Santosh, M., Tsunogae, T., Ohyama, H. Sato, K., Li, J.H., and Liu, S.J., 2008, Carbonic metamorphism at ultrahigh-temperatures. Earth and Planetary Science Letters 266, 149-165.
  14. ↑ Farquhar và đồng nghiệp (1996). “Preservation of oxygen isotope compositions in granulites from Northwestern Canada and Enderby Land, Antarctica: implications for high-temperature isotopic thermometry” 125 (2-3). tr. 213–224. doi:10.1007/s004100050217. Truy cập ngày 6 tháng 10 năm 2010.  Đã bỏ qua tham số không rõ |vol= (trợ giúp) Bảo trì CS1: Định rõ "và đồng nghiệp" (link)
  15. ↑ Baba, S., 1998, Proterozoic anticlockwise P-T path of the Lewisian complex of South Harris, outer Hebrides, NW Scotland: Journal of Metamorphic of Geology, v. 16, p. 819–841.
  16. ↑ Baba, S., 1999, Sapphirine-bearing orthopyroxene-kyanite/sillimanite granulites from South Harris, NW Scotland: Evidence for Proterozoic UHT metamorphism in the Lewisian: Contributions to Mineralogy and Petrology, v. 136, p. 33–47.
  17. ↑ Baba, S., 2003, Two stages of sapphirine formation during prograde and retrograde metamorphism in the Paleoproterozoic Lewisian complex in South Harris, NW Scotland: Journal of Petrology, v. 44, p. 329–354.
  18. ↑ Hollis, J. A., Harley, S. L., White, R. W., and Clarke, G. L., 2006, Preservation of evidence for prograde metamorphism in UHT HP granulites, South Harris, Scotland: Journal of Metamorphic Geology, v. 24, p. 263–279.
  19. ↑ Dasgupta, S., Sanyal, S., Sengupta, P., and Fukuoka, M.,1994, Petrology of granulites from Anakapalle-evidence for Proterozoic decompression in the Eastern Ghats, India: Journal of Petrology, v. 35, p. 433–459.
  20. ↑ Motoyoshi, Y., and Ishikawa, M., 1997, Metamorphic and structural evolution of granulites from Rundvågshetta,Lützow-Holm Bay, east Antarctica, in Ricci, C. A., ed., The Antarctic region: Geological evolution and processes: Proceedings of the VII International Symposium on the Antarctic Earth Sciences, Siena, Terra Antarctica, p. 65–72.
  21. ↑ Sajeev, K. and Osanai, Y. 2004a, Ultrahigh-temperature Metamorphism (1150°C and 12 kbar) and Multi-stage Evolution of Mg-Al Granulites from Central Highland Complex, Sri Lanka, Journal of Petrology, v. 45, p. 1821-1844.
  22. ↑ Sajeev, K. and Osanai, Y. 2004b, 'Osumilite' and 'spinel+quartz' from Highland Complex, Sri Lanka: a case of cooling and decompression after ultrahigh-temperature metamorphism. Journal of Mineralogical and Petrological Sciences (JMPS), v.99, p. 320-327.
  23. ↑ Sajeev, K., Osanai, Y., Connolly, J.A.D., Suzuki, S. Ishioka, J., Kagami H. and Rino S. 2007, Extreme Crustal Metamorphism during a Neoproterozoic Event in Sri Lanka: A Study of Dry Mafic Granulites. Journal of Geology v. 115, p. 563–582.
  24. ↑ Brown, M., and Raith, M., 1996, First evidence of ultrahigh-temperature decompression from the granulite province of Southern India: Journal of the Geological Society, London, v. 153, p. 819–822.
  25. ↑ Morimoto, T., Santosh, M., Tsunogae, T., and Yoshimura, Y., 2004, Spinel + quartz association from the Kerala khondalites, southern India: Evidence for ultrahightemperature metamorphism: Journal of Mineralogical and Petrological Sciences, v. 99, p. 257–278.
  26. ↑ Tateishi, K., Tsunogae, T., Santosh, M. and Janardhan, A.S., 2004, First report of sapphirine+ quartz assemblage from southern India: Implications for ultrahigh- temperature metamorphism. Gondwana Research 7, 899-912.
  27. ↑ Sajeev, K., Osanai, Y. and Santosh, M. 2004, Ultrahigh-temperature metamorphism followed by two-stage decompression of garnet-orthopyroxene-sillimanite granulites from Ganguvarpatti, Madurai block, southern India. Contributions to Mineralogy and Petrology, v. 148, p. 29-46.
  28. ↑ Sajeev, K., Santosh, M. and Kim, H.S. 2006, Partial melting and P-T evolution of the Kodaikanal Metapelite Belt, southern India. Lithos v. 92, p. 465-483.
  29. ↑ Santosh, M., Sajeev, K., 2006. Anticlockwise evolution of ultrahigh-temperature granulites within continental collision zone in southern India. Lithos 92, 447–464.
  30. ↑ Shimpo, M., Tsunogae, T., Santosh, M., 2006. First report of garnet–corundum rocks from southern India: implications for prograde high-pressure (eclogite-facies?)metamorphism. Earth and Planetary Science Letters 242, 111–129.
  31. ↑ Prakash,D., Arima, M.and Mohan, A.2006, UHT metamorphism in the Palni Hills, South India: Insights from feldspar thermometry and phase equilibria. International Geology Review, v. 48, pp. 619-638.
  32. ↑ Prakash,D., Arima,M. and Mohan,A. 2007, Ultrahigh-temperature mafic granulites from Panrimalai, South India: Constraints from phase equilibria and thermobarometery. Journal of Asian Earth Sciences, v. 29, pp. 41-61.
  33. ↑ Osanai, Y., Nakano, N., Owada, M., Nam, T. N., Toyoshima, T., Tsunogae, T., and Binh, P. (2004). “Permo-Triassic ultrahigh-temperature metamorphism in the Kontum Massif, central Viet Nam”. Journal of Mineralogical and Petrological Sciences 99: 225–241. Truy cập ngày 7 tháng 10 năm 2010.  Đã bỏ qua tham số không rõ |vol= (trợ giúp)
  34. ↑ Osanai, Y., Owada, M., Kamei, A., Hamamoto, T., Kagami, H., Toyoshima, T., Nakano N. and Nam T.N. 2006, The Higo metamorphic complex in Kyushu, Japan as the fragment of Permo–Triassic metamorphic complexes in East Asia. Gondwana Research, v. 9, p. 152-166.
  35. ↑ Dunkley, D.J., Suzuki, K., Hokada, T., Kusiak, M.A., 2008, Contrasting ages between isotopic chronometers in granulites: Monazite dating and metamorphism in the Higo Complex, Japan, Gondwana Research, doi:10.1016/j.gr.2008.02.003.
  36. ↑ Droop, G. T. R., and Bucher-Nurminen, K., 1984, Reaction textures and metamorphic evolution of sapphirine-bearing granulites from the Gruf Complex, Italian Central Alps: Journal of Petrology, v. 25, p. 766–803.

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