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Volumn 44, Issue 24, 1999, Pages 2295-2298

Could tectonic overpressure cause ultrahigh-pressure metamorphism?

Author keywords

Plastic deformation; Tectonic overpressure; Ultrahigh pressure

Indexed keywords


EID: 5544315207     PISSN: 10016538     EISSN: None     Source Type: Journal    
DOI: 10.1007/BF02885943     Document Type: Review
Times cited : (3)

References (11)
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  • 2
    • 5544254887 scopus 로고    scopus 로고
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  • 3
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    • Dobrzhineskaya, L.1    Green, H.W.2    Wang, S.3
  • 4
    • 0006143161 scopus 로고    scopus 로고
    • Is the depth where UHP rocks were formed in the Dabie Mountains limited to 100-150 km?
    • Jin, Z., Jin, S., Gao, S. et al., Is the depth where UHP rocks were formed in the Dabie Mountains limited to 100-150 km? Chinese Science Bulletin, 1998, 43: 767.
    • (1998) Chinese Science Bulletin , vol.43 , pp. 767
    • Jin, Z.1    Jin, S.2    Gao, S.3
  • 5
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    • Haggerty, S.E.1    Sauter, V.2
  • 6
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    • Sauter, V., Haggerty, S. E., Field, S., Ultra-deep (> 300 km) ultramafic xenolith: new petrologic evidence from the transition zone, Science, 1991, 252: 827.
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    • Sauter, V.1    Haggerty, S.E.2    Field, S.3
  • 7
    • 0041609399 scopus 로고
    • A redetermination of equilibrium relations between kyanite and sillimanite
    • Clark, S. P., A redetermination of equilibrium relations between kyanite and sillimanite, Am. J. Sci., 1961, 259: 641.
    • (1961) Am. J. Sci. , vol.259 , pp. 641
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    • Flow properties of continental lithosphere
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  • 10
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  • 11
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.