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Title: Progressive carbonation of high-Mg basalts during greenschist metamorphism, Victory Gold Mine, Kambalda, Western Australia

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6611147

Mapping of inferred reaction isograds developed during regional greenschist metamorphism indicates progressive carbonation of the regional invariant assemblage of epidote-biotite-actinolite-albite-quartz-muscovite-ilmenite-sphene-magnetite. The initial stage of carbonation involves the replacement of actinolite and epidote by chlorite, calcite and biotite. Further carbonation converts aggregates of sphene, ilmenite and magnetite to rutile, carbonate and quartz. In extreme carbonation, chlorite and biotite are replaced by dolomite, muscovite and quartz. The degree of progressive carbonation increases with increasing intensity of foliation development; primary igneous textures are preserved in uncarbonated domains. Mineral reactions have been modeled in the system SiO/sub 2/-Al/sub 2/O/sub 3/-MgO-CaO-Na/sub 2/O-K/sub 2/-TiO/sub 2/-H/sub 2/O-CO/sub 2/ using mineral compositions determined by microprobe analyses. Equilibria at isograd surfaces indicate CO/sub 2/, H/sub 2/O and K/sub 2/O were added and/or removed by the metamorphic fluid. The ratio of CO/sub 2/ to H/sub 2/O in the metamorphic fluid was buffered by the mineral assemblage in low strain areas, whereas the assemblages of rocks developing the schist zones can be explained by an increase in the ratio of CO/sub 2/ to H/sub 2/O in the fluid toward the center of these zones. In a practical sense the mineral equilibrium may aid in mapping and interpreting areas of regional carbonation in metabasites and aid in the delineation of structures related to concentrations of gold.

Research Organization:
Western Mining Corporation, Kambalda (Australia)
OSTI ID:
6611147
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English