Origin of heterogeneous mafic enclaves by two-stage hybridisation in magma conduits (dykes) below and in granitic magma chambers

Special Paper of the Geological Society of America

Volumn 350, Issue , 2000, Pages 27-45

  Collins, W J ^a   Richards, S R ^a   Healy, B E ^a   Ellison, P I ^a  

^a UNIVERSITY OF NEWCASTLE   (Australia)

Author keywords

Double enclaves; Lachlan fold belt; Magma mixing; Rheology; Synplutonic

Indexed keywords

BOUNDARY LAYERS; COMPLEX NETWORKS; FELDSPAR; GRADING; RHEOLOGY; SHEAR FLOW; SHEAR STRESS;

DOUBLE ENCLAVES; GEOCHEMICAL EVIDENCE; GRANITIC COMPOSITION; HYBRIDISATION PROCESS; LACHLAN FOLD BELTS; MAGMA MIXING; SOUTH-EASTERN AUSTRALIA; SYNPLUTONIC;

MIXING;

DIKE; GRANITE; MAFIC ROCK; MAGMA; MAGMA CHAMBER; PETROGENESIS; PLUTONIC ROCK; RHEOLOGY;

AUSTRALIA; LACHLAN FOLD BELT;

EID: 84859077288     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/0-8137-2350-7.27     Document Type: Conference Paper

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