Solubility of K-feldspar, muscovite and quartz at 0.5-2.5 GPa, 600-700°C with implications for mass transport in the crust

Details Solubility of K-feldspar, muscovite and quartz at 0.5-2.5 GPa, 600-700°C with implications for mass transport in the crust Solubility of K-feldspar, muscovite and quartz at 0.5-2.5 GPa, 600-700°C with implications for mass transport in the crust

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008gecas..72q...6a&link_type=openurl

Geochimica et Cosmochimica Acta, Volume 72, Issue 12, p.A6

Physics

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