Physical controls of magmatic productivity at Pacific-type convergent margins: Numerical modelling

Physics of the Earth and Planetary Interiors

Volumn 163, Issue 1-4, 2007, Pages 209-232

  Gorczyk, Weronika ^a   Willner, Arne P ^b   Gerya, Taras V ^a   Connolly, James A D ^a   Burg, Jean Pierre ^a  

^a ETH ZURICH   (Switzerland)

^b RUHR UNIVERSITY BOCHUM   (Germany)

Author keywords

Active margin; Back arc spreading; Magmatic productivity; Mantle wedge melting; Numerical modelling; Slab retreat

Indexed keywords

COMPUTER SIMULATION; PETROLOGY; STRUCTURAL GEOLOGY;

MAGMATIC PRODUCTIVITY; MANTLE FLOW; PETROLOGICAL-THERMOMECHANICAL MODEL; SUBDUCTION;

TECTONICS;

ACCRETIONARY PRISM; ACTIVE MARGIN; CONVERGENT MARGIN; FOREARC BASIN; MAGMATIC DIFFERENTIATION; MESOZOIC; NUMERICAL MODEL; PALEOZOIC; PLATE BOUNDARY; PLATE CONVERGENCE; SLAB; SPREADING CENTER; SUBDUCTION ZONE;

CHILE; PACIFIC OCEAN; SOUTH AMERICA;

EID: 34547877202     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2007.05.010     Document Type: Article

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