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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

✍ Scribed by Karen Rickers; Rainer Thomas; Wilhelm Heinrich


Publisher
Springer
Year
2006
Tongue
English
Weight
564 KB
Volume
41
Category
Article
ISSN
0026-4598

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