Distinct basement terranes identified from granite geochemistry in late Archaean granite-greenstones, Yilgarn Craton, Western Australia

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Hidden basement terranes have been identified by a geochemical study of granites that intrude deformed greenstones in the Eastern Goldfields of the Yilgarn Craton. The granites are calc-alkaline rocks with a high average silica content (72.5 wt%), lie mainly in the compositional range of granodiorite to monzogranite, and are derived from melting of pre-existing sialic crust. The greenstones comprise several tectono-stratigraphic terranes that were essentially assembled before intrusion of the granites. The distribution of granite types generally shows no spatial relationship to these terranes or to terrane boundary faults. The Emu Fault, which separates the Kurnalpi Terrane to the east, from the Kalgoorlie and Gindalbie terranes to the west, provides an exception. Granites to the east of this fault have lower TiO 2, FeO 2 and MgO, and generally higher Na 2O, compared to granites to the west. These contrasting compositions result from differences within the source regions and are interpreted to reflect two distinct basement terranes. The basement terrane beneath the Kurnalpi region had a higher proportion of tonalite than was present beneath the Kalgoorlie and Gindalbie terranes. We suggest that a regional tonalite-trondhjemite-granodiorite basement was accreted prior to complete accumulation of the greenstones and was later recycled, to form the granites. The Emu Fault is inferred to reflect a suture in the underlying basement of the greenstones.