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Volumn 144, Issue 1, 2001, Pages 221-230

Azimuthal variation of the P phase in Icelandic receiver functions

Author keywords

Crust; Iceland; P waves; Ridge; Wave propagation; Waveform ana

Indexed keywords

AZIMUTH; P-WAVE; SEISMIC VELOCITY; TELESEISMIC WAVE; VELOCITY STRUCTURE;

EID: 0035122762     PISSN: 0956540X     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.0956-540X.2000.01290.x     Document Type: Article
Times cited : (4)

References (24)
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    • Flovenz, O.G.1
  • 11
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    • Seismic structure of the lithosphere from teleseismic converted arrivals observed at small arrays in the southern Sierra Nevada and vicinity, California
    • (1998) J. Geophys. Res , vol.103 , pp. 10065-10090
    • Jones, C.H.1    Phinney, R.A.2
  • 12
    • 0018655880 scopus 로고
    • Structure under mount rainier, Washington, inferred from teleseismic body waves
    • (1979) J. Geophys. Res , vol.84 , pp. 4749-4762
    • Langston, C.A.1
  • 13
  • 20
    • 0002164891 scopus 로고
    • Subaerial volcanism in the western North Atlantic
    • The Western North Atlantic Region. eds Vogt, P.E. & Tucholke, B.E. Geol. Soc. Am., Boulder
    • (1986) The Geology of North America , vol.M , pp. 69-86
    • Sæmundsson, K.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.