Abstract
Small Archaean, pre-metamorphic layered sill-like intrusions showing “ Stillwatertype” differentiation are widespread in the Eastern Goldfields region of Western Australia. The sills have undergone low-grade metamorphism, but the retention of some original minerals and excellent preservation of primary textures have enabled most of their original features to be reconstructed. Despite their small size in comparison with well known layered intrusions, simple differentiation sequences are developed ranging upwards from dunite and harzburgite through orthopyroxenite, norite, norite-gabbro and gabbro to granophyre and anorthosite. The parent magma for the sills appears to have been rich in MgO (15–18%) and is probably represented by the spatially associated high-Mg basalts found in the region. The complexes are interpreted as being contemporaneous with volcanism and may be high-level emplacements.
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Williams, D.A.C., Hallberg, J.A. Archaean layered intrusions of the Eastern Goldfields region, Western Australia. Contr. Mineral. and Petrol. 38, 45–70 (1973). https://doi.org/10.1007/BF00371726
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DOI: https://doi.org/10.1007/BF00371726