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P‐T‐X (CO 2 ) conditions in mafic and calc‐silicate hornfelses from Oberon, New South Wales, Australia
Author(s) -
ANDREW A. S.
Publication year - 1984
Publication title -
journal of metamorphic geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.639
H-Index - 114
eISSN - 1525-1314
pISSN - 0263-4929
DOI - 10.1111/j.1525-1314.1984.tb00293.x
Subject(s) - geology , geochemistry , mafic , amphibole , metamorphism , phlogopite , hornfels , actinolite , plagioclase , cordierite , skarn , diopside , epidote , fluid inclusions , quartz , biotite , chlorite , chemistry , mantle (geology) , paleontology , biochemistry , catalysis
The Rockley Volcanics from near Oberon, New South Wales occur within the aureole of the Carboniferous Bathurst Batholith and have been contact metamorphosed at P ∼ 100 ± 50MPa (10.5kbar) and a maximum T ∼ 565°C in the presence of a C–O–H fluid. Prior to contact metamorphism the volcanics were regionally metamorphosed and altered with the extensive development of actinolite, chlorite, plagioclase, quartz and calcite. The contact metamorphosed equivalents of these rocks have been subdivided into: Ca‐poor (cordierite + gedrite), Mg‐rich (amphibole + olivine + spinel), mafic (amphibole + plagioclase) and Ca‐rich (amphibole + garnet + diopside; diopside + plagioclase; garnet + diopside + wollastonite) rocks. The chemistry of the minerals in the hornfelses was controlled by the bulk rock chemistry and fluid composition. Pargasites and hastingsites as well as an unusual phlogopite with blue green pleochroism, are found in Ca‐rich hornfelses. A comparison of the assemblages with experimentally derived equilibria suggests that the fluid phase associated with the Ca‐rich hornfelses was water‐rich (X co2 = 0.1 to 0.3) while that associated with the Mg‐rich hornfelses was enriched in CO 2 (X co2 > 0.7). The different hornfels types have reacted to contact metamorphism independently in both their solid and fluid chemistries.