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Volumn 35, Issue 4, 2002, Pages 477-488

The structure of the crust and upper mantle to depths of 320 km beneath the Kaapvaal craton, from P wave arrivals generated by regional earthquakes and mining-induced tremors

Author keywords

Kaapvaal craton; Seismic wavespeed

Indexed keywords

CRUSTAL STRUCTURE; CRUSTAL THICKNESS; EARTHQUAKE; P-WAVE; SEISMICITY; TRAVEL TIME; UPPER MANTLE;

EID: 0036881626     PISSN: 08995362     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0899-5362(02)00157-4     Document Type: Article
Times cited : (24)

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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.