Petrology and crystal chemistry of the Ruby Star granodiorite, Pima County, Arizona

作者: Nancy Jane Hess

DOI:

关键词:

摘要: The Laramide -aged Ruby Star batholith consists of an outer equigranular granodiorite rim and inner porphyritic core. A quartz monzonite stock breaches the southern together with discontinuous bodies biotite diorite host Sierrita -Esperanza porphyry copper deposit. whole rock data indicate that crystallized at 650 to 700 C a fH2O 1800 2000 bars. Analyses show Mg enrichmentin simultaneous Fe enrichment in rock. These trends presence magnetite suggest high increasing f02. dehydration reaction Czamanske Wones (1973) suggests crystallization occurred f02 10 -1' -56 bars 750 C. temperature -f02 conditions match those required for hydrothermal fluids carry sulphur species complex (Burnham Ohmoto, 1 98$) .

参考文章(37)
S. Ludington, The biotite-apatite geothermometer revisited American Mineralogist. ,vol. 63, pp. 551- 553 ,(1978)
David R. Wones, Franklin C. W. Dodge, The Stability of Phlogopite in the Presence of Quartz and Diopside Springer Netherlands. pp. 229- 247 ,(1977) , 10.1007/978-94-010-1252-2_12
Allan R. Chivas, Geochemical evidence for magmatic fluids in porphyry copper mineralization Contributions to Mineralogy and Petrology. ,vol. 78, pp. 389- 403 ,(1982) , 10.1007/BF00375201
Richard E. Beane, Biotite Stability in the Porphyry Copper Environment Economic Geology. ,vol. 69, pp. 241- 256 ,(1974) , 10.2113/GSECONGEO.69.2.241
William C. Luth, Richard H. Jahns, O. Frank Tuttle, The granite system at pressures of 4 to 10 kilobars Journal of Geophysical Research. ,vol. 69, pp. 759- 773 ,(1964) , 10.1029/JZ069I004P00759