The growth interval of garnet in the UHP eclogites from the Dabie orogen, China

American Mineralogist

Volumn 96, Issue 8-9, 2011, Pages 1300-1307

  Cheng, Hao ^a   Vervoort, Jeffrey D ^b   Li, Xianhua ^c   Zhang, Chao ^a   Li, Qiuli ^c   Zheng, Shu ^d  

^a TONGJI UNIVERSITY   (China)

^b WASHINGTON STATE UNIVERSITY   (United States)

^c INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^d CHINA UNIVERSITY OF GEOSCIENCES   (China)

Author keywords

Garnet; Lu Hf; U Pb; Zircon

Indexed keywords

BINARY ALLOYS; FELDSPAR; GEOCHRONOLOGY; HAFNIUM ALLOYS; LEAD ALLOYS; LUTETIUM ALLOYS; PROBABILITY DISTRIBUTIONS; RARE EARTHS; TRACE ELEMENTS; ZIRCON;

AMPHIBOLITE FACIES; HIGH SPATIAL RESOLUTION; MAJOR AND TRACE ELEMENTS; METAMORPHIC GROWTH; TIME INTERVAL; U-PB GEOCHRONOLOGY; ULTRA-HIGH-PRESSURE ECLOGITE; WEIGHTED MEAN;

GARNETS;

CATHODOLUMINESCENCE; ECLOGITE; FELDSPAR; GARNET; GEOCHRONOLOGY; HAFNIUM; LUTETIUM; OMPHACITE; RARE EARTH ELEMENT; SPATIAL DISTRIBUTION; TRACE ELEMENT; ULTRAHIGH PRESSURE METAMORPHISM; URANIUM-LEAD DATING; ZIRCON;

CHINA;

EID: 80053235798     PISSN: 0003004X     EISSN: 19453027     Source Type: Journal    
DOI: 10.2138/am.2011.3737     Document Type: Article

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