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Volumn 23, Issue 14, 1996, Pages 1821-1824

Rheological control of oceanic crust separation in the transition zone

Author keywords

[No Author keywords available]

Indexed keywords

GARNETS; BOUNDARY CONDITIONS; BUOYANCY; DENSITY (SPECIFIC GRAVITY); GEOCHEMISTRY; MATHEMATICAL MODELS; MINERALS; NUMERICAL METHODS; RHEOLOGY; VISCOSITY;

EID: 0030184126     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/96GL01594     Document Type: Article
Times cited : (74)

References (13)
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    • Compositional vs. thermal buoyancy and the evolution of subducted lithosphere
    • Gaherty, J.B., and B.H. Hager, Compositional vs. thermal buoyancy and the evolution of subducted lithosphere. Geophys. Res. Lett., 21, 141-144, 1994.
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    • Gaherty, J.B.1    Hager, B.H.2
  • 5
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    • Hansen, U., and D.A. Yuen, Effects of depth-dependent thermal expansivity on the interaction of thermal-chemical plumes with a compositional boundary, Phys. Earth Planet. Inter., 86, 205-221, 1994.
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    • Hansen, U.1    Yuen, D.A.2
  • 7
    • 0029518747 scopus 로고
    • TEM observations of several spinel-garnet assemblies: Toward the rheology of the transition zone
    • Ingrin, J., and M. Madon, TEM observations of several spinel-garnet assemblies: toward the rheology of the transition zone, Terra Nova, 7, 509-515, 1995.
    • (1995) Terra Nova , vol.7 , pp. 509-515
    • Ingrin, J.1    Madon, M.2
  • 8
    • 0027455973 scopus 로고
    • Phase transformation in subducted oceanic crust and buoyancy relationships at depths of 600-800 km in the mantle
    • Irifune, T., and A.E. Ringwood, Phase transformation in subducted oceanic crust and buoyancy relationships at depths of 600-800 km in the mantle, Earth Planet. Science Lett., 117, 101-110, 1993.
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  • 9
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    • Karato, S.1
  • 10
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  • 11
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  • 12
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  • 13
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.