Formation of high-Mg diorites through assimilation of peridotite by monzodiorite magma at crustal depths

Journal of Petrology

Volumn 51, Issue 7, 2010, Pages 1381-1416

  Qian, Qing ^a,b   Hermann, Jörg ^b  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

High Mg diorite; Intra continental; North China block; Sanukitoid; Trace element

Indexed keywords

ANATEXIS; CHEMICAL COMPOSITION; CRUST-MANTLE BOUNDARY; CRUSTAL EVOLUTION; CRYSTALLIZATION; DIORITE; EMPLACEMENT; FORMATION MECHANISM; FRACTIONATION; IGNEOUS GEOCHEMISTRY; MAGMA ASSIMILATION; MAGNESIUM; MONZONITE; PARTIAL MELTING; PERIDOTITE; PETROLOGY; RARE EARTH ELEMENT; XENOLITH;

CHINA; NORTH CHINA BLOCK;

EID: 77954350600     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egq023     Document Type: Article

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