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Volumn 329, Issue 1-4, 2000, Pages 171-191

Structure of the makran subduction zone from wide-angle and reflection seismic data

Author keywords

Convergent margins; Makran; Refraction seismics; Underplating

Indexed keywords

ACCRETIONARY PRISM; PLATE BOUNDARY; SEISMIC REFLECTION; SEISMIC SURVEY; SUBDUCTION ZONE; UNDERPLATING;

EID: 0035044182     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(00)00195-5     Document Type: Article
Times cited : (224)

References (27)
  • 9
    • 0030456176 scopus 로고    scopus 로고
    • Paleogeographic and paleotectonic evolution of the Himalayan Range as reflected by detrital modes of Tertiary sandstones and modern sands (Indus transect, India and Pakistan)
    • (1996) GSA Bull , vol.108 , pp. 631-642
    • Garzanti, E.1    Critelli, S.2    Ingersoll, R.V.3
  • 25
    • 0001187714 scopus 로고
    • The Makran continental margin: Structure of a thickly sedimented convergent plate boundary. Studies in continental margin geology
    • Watkinsand, J.S., Drake, C.L. (Eds.)
    • (1983) Mem. Am. Ass. Petrol. Geol , vol.34 , pp. 499-518
    • White, R.S.1    Louden, K.E.2
  • 26


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.