Subducted upper and lower continental crust contributes to magmatism in the collision sector of the Sunda-Banda arc, Indonesia

Geology

Volumn 32, Issue 1, 2004, Pages 41-44

  Elburg, M A ^a,b   van Bergen, M J ^c   Foden, J D ^b  

^a MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

^b UNIVERSITY OF ADELAIDE   (Australia)

^c UTRECHT UNIVERSITY   (Netherlands)

Author keywords

Collision; Indonesia; Pb 206 Pb 204; Subduction; Sunda Banda arc

Indexed keywords

LITHOSPHERE; OCEAN ISLAND BASALTS (OIB); SUBDUCTION SYSTEMS;

BASALT; HELIUM; IGNEOUS ROCKS; ISOTOPES; LEAD; SEDIMENTS;

GEOLOGY;

COLLISION ZONE; CONTINENTAL CRUST; PLATE TECTONICS; SUBDUCTION;

BANDA ARC; INDONESIAN SEAS; PACIFIC OCEAN; SUNDA ARC;

EID: 1142268934     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/G19941.1     Document Type: Article

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