Calc-alkaline lamprophyres from Lusatia (Germany)-Evidence for a repeatedly enriched mantle source

Chemical Geology

Volumn 353, Issue , 2013, Pages 230-245

  Abdelfadil, Kh M ^a   Romer, R L ^a   Seifert, Th ^b   Lobst, R ^c  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^b TU BERGAKADEMIE FREIBERG   (Germany)

^c Landwirtschaft und Geologie   (Germany)

Author keywords

Mantle metasomatism; Spessartite; Tholeiitic gabbro; Variscan orogeny

Indexed keywords

CONTINENTAL CRUSTS; ISOTOPIC COMPOSITION; LITHOSPHERIC MANTLE; MANTLE METASOMATISM; ND ISOTOPIC COMPOSITIONS; SPESSARTITE; THOLEIITIC GABBRO; VARISCAN OROGENIES;

ISOTOPES; LEAD;

NEODYMIUM;

CADOMIAN OROGENY; CALC ALKALINE ROCK; GABBRO; HERCYNIAN OROGENY; ISOTOPIC RATIO; LAMPROPHYRE; LEAD ISOTOPE; LITHOSPHERIC STRUCTURE; MANTLE SOURCE; MANTLE STRUCTURE; METASOMATISM; SPESSARTINE; STRONTIUM ISOTOPE; THOLEIITE;

ERZGEBIRGE MOUNTAINS; GERMANY; LUSATIA; SUDETES;

EID: 84883657532     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.10.023     Document Type: Article

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