Geochemical and Nd-Hf isotopic constraints on the origin of the ~ 1.74-Ga Damiao anorthosite complex, North China Craton

Lithos

Volumn 113, Issue 3-4, 2009, Pages 673-690

  Zhao, Tai Ping ^a,b   Chen, Wei ^a,c   Zhou, Mei Fu ^b  

^a GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^b UNIVERSITY OF HONG KONG   (Hong Kong)

^c UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

Author keywords

High Al gabbro; Mangerite; Massif type anorthosite; North China Craton; Post collisional magmatism; Proterozoic

Indexed keywords

ANORTHOSITE; ARCHEAN; CRYSTALLIZATION; DIKE SWARM; DIORITE; EMPLACEMENT; HAFNIUM; IGNEOUS GEOCHEMISTRY; ISOTOPIC ANALYSIS; ISOTOPIC COMPOSITION; LITHOLOGY; MAGMA CHAMBER; MAGMATIC DIFFERENTIATION; MAGMATISM; MELTING; NEODYMIUM ISOTOPE; PROTEROZOIC; RARE EARTH ELEMENT; ZIRCON;

ASIA; CANADA; CHINA; EURASIA; FAR EAST; HARP LAKE; LARAMIE; NORTH AMERICA; NORTH CHINA BLOCK; ONTARIO [CANADA]; UNITED STATES; WYOMING;

EID: 70449089111     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2009.07.002     Document Type: Article

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