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The Albany Fraser Orogen is located along the southern and southeastern margins of the Archean Yilgarn Craton. The orogen formed during reworking of the Yilgarn Craton, along with variable additions of juvenile mantle material, from at least 1810Ma to 1140Ma. The Fraser Zone is a 425km long and 50km wide geophysically distinct belt near the northwestern edge of the orogen, hosting abundant sills of...
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