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Volumn 151, Issue 1, 2002, Pages 132-145

The P wavespeed structure below and around the Kaapvaal craton to depths of 800 km, from traveltimes and waveforms of local and regional earthquakes and mining-induced tremors

Author keywords

Kaapvaal craton; Seismic wavespeeds; Transition zone; Upper mantle

Indexed keywords

CRATON; P-WAVE; SEISMIC VELOCITY; UPPER MANTLE; VELOCITY STRUCTURE;

EID: 0036787083     PISSN: 0956540X     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-246X.2002.01751.x     Document Type: Article
Times cited : (32)

References (30)
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    • Elastic wave velocities of forsterite and its spinel form and chemical boundary hypothesis for the 410 km discontinuity
    • (1998) J. Geophys. Res , vol.103 , pp. 9591-9608
    • Fujisawa, H.1
  • 18
    • 0010536768 scopus 로고
    • A study of the effect of Q on the observation of upper mantle travel-time branches using adaptive processing techniques
    • ed. Beauchamp, K.G., Proceedings of NATO Advanced Study held at Sandefjord, Norway, April 22-May 3, 1974, Noordhoff, Leiden, The Netherlands
    • (1975) Exploitation of Seismograph Networks , pp. 471-488
    • Mereu, R.F.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.