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Volumn 203, Issue 3-4, 2002, Pages 925-935

Dynamic interaction of cold anomalies with the mid-ocean ridge flow field and its implications for the Australian-Antarctic Discordance

Author keywords

AAD; Dynamic flow; Rifting; Subsidence; Thermal anomalies; Viscosity

Indexed keywords

ANOMALY; ASTHENOSPHERE; BUOYANCY; CONTINENTAL BREAKUP; MID-OCEAN RIDGE; THERMAL CONVECTION; VISCOSITY;

EID: 0037110562     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(02)00948-2     Document Type: Article
Times cited : (12)

References (31)
  • 2
  • 5
    • 0033559995 scopus 로고    scopus 로고
    • Effect of near-ridge thermal anomalies on the subsidence of the oceanic lithosphere: Constraints from a 2-D dynamic model
    • (1999) Geophys. Res. Lett , vol.26 , pp. 807-810
    • Chiao, L.Y.1    Wang, C.W.2
  • 6
    • 0035822056 scopus 로고    scopus 로고
    • Reykjanes 'V'-shaped ridges originating from a pulsing and dehydrating mantle plume
    • (2001) Nature , vol.411 , pp. 681-684
    • Ito, G.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.