The behavior of trace elements during the chemical evolution of the H2O-, B-, and F-rich granite-pegmatite-hydrothermal system at Ehrenfriedersdorf, Germany: A SXRF study of melt and fluid inclusions

Mineralium Deposita

Volumn 41, Issue 3, 2006, Pages 229-245

  Rickers, Karen ^a,b   Thomas, Rainer ^b   Heinrich, Wilhelm ^b  

^a DESY   (Germany)

^b GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

Author keywords

Ehrenfriedersdorf; Fluid inclusions; Germany; Melt inclusions; Sn W deposit; Synchrotron radiation XRF

Indexed keywords

FLUID INCLUSION; GRANITE; HYDROTHERMAL SYSTEM; IGNEOUS GEOCHEMISTRY; MELT INCLUSION; PEGMATITE; TRACE ELEMENT;

CENTRAL EUROPE; EHRENFRIEDERSDORF; EURASIA; EUROPE; GERMANY; SAXONY;

EID: 33646895617     PISSN: 00264598     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00126-006-0057-7     Document Type: Article

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