The evidence from inclusions in pumices for the direct degassing of volatiles from the magma to the hydrothermal fluids in the Okinawa Trough
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Springer Science and Business Media LLC
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http://link.springer.com/content/pdf/10.1007/s11802-002-0014-8.pdf
Reference19 articles.
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3. Gerlach, T. M., 1989. Degassing of carbon dioxide from basaltic magma at spreading centers: mid-oceannic ridge basalts. J. Volcano. Geotherm. Res., 39: 221–232.
4. Halbach, P., B. Pracejus, and A. Marten, 1993. Geology and mineralogy of massive sulfide ores from the central Okinawa Trough. Japan. Econ. Geol., 88: 2210–2225.
5. Hedenquist, J. W., and J. B. Lowenstern, 1994. The role of magma in the formation of hydrothermal deposits. Nature, 370: 519–527.
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