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- W2005473000 abstract "Three samples were taken from the Narryer Terrane of the Yilgarn Craton. Granitic gneiss (SO2_7a) consisted largely of quartz, feldspar, biotite and muscovite. Quartz and feldspar domains define a gneissosity, and the rarer biotite and muscovite is roughly aligned parallel to this fabric. A sample of a lens of pelitic schist (SO2_8) that outcrops within granitic gneiss of the Narryer Terrane contains one foliation that consists of biotite and minor feldspar and quartz. Biotite wraps around pseudomorphed porphyroblasts interpreted to be andalusite (Fig. 2a). Andalusite is replaced by very fine-grained mats of sericite and quartz (Fig. 2a). If the andalusite crystallised in the amphibolite facies, then the biotite foliation may have formed in either the amphibolite or greenschist facies (i.e. on the prograde or retrograde path) given that the andalusite porphyroblasts are relatively undeformed but are wrapped by the biotite foliation. The randomly oriented sericite may have crystallised during a greenschist facies retrograde metamorphic event after deformation had ceased. Sample SO2_2a is from an even-grained undeformed biotite granite that intrudes surrounding Archaean granitic gneiss and comprises mainly quartz, feldspar, muscovite, and biotite. Foliations in samples SO2_7a and SO2_8 are thought to have formed during an Archaean deformation and high-grade metamorphic event (Occhipinti & Sheppard 2001) based on regional structural and metamorphic correlations, and the presence of unfoliated c. 2600 Ga granite sheets and plutons that cut these fabrics in the region. However, the retrograde, unfoliated sericite present in sample SO2_8 could have formed at any time after this Archaean deformation and metamorphism event." @default.
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- W2005473000 date "2009-01-01" @default.
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- W2005473000 title "Neoproterozoic reworking of the Palaeoproterozoic Capricorn Orogen of Western Australia and implications for the amalgamation of Rodinia" @default.
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- W2005473000 doi "https://doi.org/10.1144/sp327.18" @default.
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