The return of sialic material to the mantle indicated by terrigeneous material subducted at convergent margins

Tectonophysics

Volumn 219, Issue 1-3, 1993, Pages 163-175

  von Huene, R ^a   Scholl, D W ^b  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b U S GEOLOGICAL SURVEY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ACCRETION; CONVERGENT MARGIN; MANTLE; MANTLE EVOLUTION; PLATE MARGIN; SEDIMENT UNDERTHRUSTING; SIALIC MATERIAL; SUBDUCTION;

EID: 0027388652     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(93)90294-T     Document Type: Article

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