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Volumn 143, Issue 1, 2000, Pages 230-238

Effect of the viscoelastic lithosphere on polar wander speed caused by the Late Pleistocene glacial cycles

Author keywords

Earth's rotation; Lithosphere; Mantle viscosity; Maxwell viscoelasticity; Polar wander

Indexed keywords

GLACIATION; LITHOSPHERIC STRUCTURE; PLEISTOCENE; POLAR WANDERING; VISCOELASTICITY;

EID: 0033790846     PISSN: 0956540X     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-246X.2000.00233.x     Document Type: Article
Times cited : (10)

References (28)
  • 6
    • 0032861998 scopus 로고    scopus 로고
    • Implications of a non-adiabatic density gradient for the Earth's viscoelastic response to surface loading
    • (1999) Geophys. J. Int. , vol.137 , pp. 663-674
    • Nakada, M.1
  • 11
    • 0022213132 scopus 로고
    • The LAGEOS constraint on deep mantle viscosity: Results from a new normal mode method for the inversion of viscoelastic relaxation spectra
    • (1985) J. Geophys. Res. , vol.90 , pp. 9411-9421
    • Peltier, W.R.1
  • 14
    • 0021644435 scopus 로고
    • Postglacial rebound observed by LAGEOS and the effective viscosity of the lower mantle
    • (1984) J. Geophys. Res. , vol.89 , pp. 1977-1087
    • Rubincam, D.P.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.