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Volumn 83, Issue 45, 2002, Pages

PLUME investigates south pacific superswell

Author keywords

[No Author keywords available]

Indexed keywords


EID: 3042765667     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2002EO000354     Document Type: Article
Times cited : (28)

References (12)
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  • 2
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  • 3
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    • Debayle, E.1    Kennett, B.L.N.2
  • 4
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    • Flattening of the oceanic topography and geoid : Thermal versus dynamic origin
    • Doin, M. P, and L Fleitout, Flattening of the oceanic topography and geoid:Thermal versus dynamic origin, Geophys. J. Int., 143, 582-594, 2000.
    • (2000) Geophys. J. Int. , vol.143 , pp. 582-594
    • Doin, M.P.1    L Fleitout2
  • 6
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    • The recrystallization front of the ronda peridotite: Evidence for melting and thermal erosion of lithospheric mantle beneath the alboran Basin
    • Lenoir, X., C. Garrido, J.-L Bodinier, J.-M. Dautria, and E. Gervilla, The recrystallization front of the Ronda peridotite: Evidence for melting and thermal erosion of lithospheric mantle beneath the Alboran basin,. J Petrol, 42, 141-158, 2001.
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  • 8
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    • McNutt, M.K.1
  • 9
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    • Mantle transition-zone structure beneath the south pacific superswell and evidence for a mantle plume underlying the society hotspot
    • Niu. F., S. C. Solomon, PG. Silver, D. Suetsugu, and H. Inoue, Mantle transition-zone structure beneath the South Pacific Superswell and evidence for a mantle plume underlying the Society hotspot, Earth Planet. Sci. Lett., 198, 371-380, 2002.
    • (2002) Earth Planet. Sci. Lett. , vol.198 , pp. 371-380
    • Niu, F.1    Solomon, S.C.2    Silver, P.G.3    Suetsugu, D.4    Inoue, H.5
  • 10
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    • Degree 12 model of shear velocity heterogeneity in the mantle.
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  • 11
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    • Viscoplastic self-consistent and equilibrium-based modeling of olivine lattice preferred orientations. Implications for the upper mantle seismic anisotropy
    • Tommasi, A., D. Mainprice, G. Canova, and Y Chastel, Viscoplastic self-consistent and equilibrium-based modeling of olivine lattice preferred orientations. Implications for the upper mantle seismic anisotropy, J. Geophys. Res., 105, 7893-7908, 2000.
    • (2000) J. Geophys. Res. , vol.105 , pp. 7893-7908
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  • 12
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    • Evidence for a stagnant plume in the transition zone?
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.