F and Cl diffusion in phonolitic melts: Influence of the Na/K ratio
Fluorine and chlorine diffusion were measured in two natural phonolitic melts, from Vesuvius (Italy) and from Laacher See (Germany), at 0.5 and 1.0 GPa, between 1250 and 1450 °C at anhydrous conditions and with about 2 and 5 wt.% of dissolved water. The two different starting materials allow us to i...
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Published in | Chemical geology Vol. 263; no. 1; pp. 89 - 98 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
15.06.2009
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Subjects | |
Online Access | Get full text |
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