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Volumn 67, Issue 3, 1997, Pages 571-582

Spatial variation in turbidite-to-contourite continuums of the Kiwada and Otadai formations in the Boso Peninsula, Japan: An unstable bottom-current system in a plio-pleistocene forearc basin

Author keywords

[No Author keywords available]

Indexed keywords

BOTTOM CURRENT; BOTTOM CURRENTS; CONTOURITE; CONTOURITES; DEEP SEA; DEEP SEA SEDIMENT; FOREARC BASIN; FOREARC BASINS; PLEISTOCENE; PLIOCENE; TURBIDITE; TURBIDITES;

EID: 0030773999     PISSN: 15271404     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (18)

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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.