Ordovician meta-pegmatite garnet (N-W Ötztal basement, Tyrol, Eastern Alps): Preservation of magmatic garnet chemistry and Sm-Nd age during mylonitization

Chemical Geology

Volumn 209, Issue 1-2, 2004, Pages 1-26

  Thoni M ^a   Miller, Ch ^b  

^a Institute of Nutritional Sciences   (Austria)

^b Institute of Mineralogy and Petrography   (Austria)

Author keywords

Early Palaeozoic events; Eastern Alps; Magmatic garnet; Meta pegmatite; Ordovician magmatism; Sm Nd garnet chronometry; Trace elements

Indexed keywords

GARNET; ISOTOPIC COMPOSITION; MAGMA CHEMISTRY; MYLONITIZATION; NEODYMIUM ISOTOPE; ORDOVICIAN; PEGMATITE; SAMARIUM; TRACE ELEMENT;

ALPS; EASTERN ALPS; EURASIA; EUROPE;

EID: 3242708430     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2004.03.006     Document Type: Article

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