Origin and geological significance of the 1.81 Ga hyalophane-rich pegmatite veins from the high-pressure granulite terrain in the Central Zone of North China Craton

Science China Earth Sciences

Volumn 55, Issue 2, 2012, Pages 193-203

  Qu, Min ^a   Guo, Jing Hui ^a   Lai, Yong ^b   Peng, Peng ^a   Liu, Fu ^a  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b Peking University   (China)

Author keywords

high pressure granulite; hyalophane; North China Craton; Paleoproterozoic; pegmatite; zircon Hf O isotope

Indexed keywords

HIGH-PRESSURE GRANULITES; HYALOPHANE; NORTH CHINA CRATON; PALEOPROTEROZOIC; PEGMATITE;

GALLIUM; GEOCHRONOLOGY; HAFNIUM; ISOTOPES; LANDFORMS; LEAD; ZIRCON;

GRANITE;

AGE DETERMINATION; CLINOPYROXENE; CRYSTALLIZATION; EPIDOTE; GRANULITE; HIGH PRESSURE; MELTING; OXYGEN ISOTOPE; PEGMATITE; PROTEROZOIC; TECTONIC SETTING; TERRAIN; TITANITE; UPLIFT; URANIUM-LEAD DATING; VEIN (GEOLOGY);

CHINA; NORTH CHINA BLOCK;

CELSIA;

EID: 84863056016     PISSN: 16747313     EISSN: None     Source Type: Journal    
DOI: 10.1007/s11430-011-4330-y     Document Type: Article

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