The composition of a primary granite-derived ore fluid from S.W. England, determined by fluid inclusion analysis

Details The composition of a primary granite-derived ore fluid from S.W. England, determined by fluid inclusion analysis The composition of a primary granite-derived ore fluid from S.W. England, determined by fluid inclusion analysis

Feb 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988gecoa..52..585b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 52, Issue 2, pp.585-588

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9

Scientific paper

Electrolyte concentrations in aqueous fluid inclusions in quartz from a high temperature hydrothermal rock have been measured for 15 elements by an improved crush-leach procedure. The primary hydrothermal fluid was dominated by NaCl and has been shown by previous studies to have been about 3 m with respect to Cl. On this basis the molar concentrations include Fe = 0.21, Mn = 0.06 and Zn = 0.02, and the fluid is interpreted as parental to some of the S.W. England ore bodies.

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