The geology of Ewarara Intrusion, Giles Complex, Central Australia

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Abstract
Ewarara is a small layered ultramafic intrusion which forms part of the Giles Complex. The flat‐lying body displays both sub‐horizontal and vertical layering, which appear to have different origins. Petrographically the intrusion consists of a lower olivine bronzitite unit and an upper pyroxenite unit. These display a small cryptic variation with the upper layer being the more iron‐rich. Many of the primary igneous textures have been destroyed by deformational effects but the intrusion retains many features of a body formed by gravity accumulation of crystals precipitating from a magma. Crystallisation of the magma is believed to have occurred near the base of the crust.
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