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- W2052490003 abstract "The Eastern Goldfields region forms part of the Yilgarn Craton which, after the Superior Province of Canada, is one of the largest fragments of Archaean granite-greenstone terrain exposed at the surface of the Earth. This craton has much in common with the more intensely studied Superior Province, but there are also significant differences between these two cratons. Both cratons were assembled from numerous smaller crustal fragments in a relatively brief period during the late Archaean. The Superior Province was assembled between 2725 and 2695 Ma (Card, 1990), and the Yilgarn Craton was assembled between c. 2670 and 2650 Ma (Myers, 1993). Both cratons contain fragments of older continental crust and volcanic arcs that formed just prior to collision and cratonisation. The Superior Province contains extensive belts of metasedimentary rocks interpreted as accretionary prisms (Card, 1990), whereas metasedimentary rocks form only a minor component of the Yilgarn Craton, and most appear to postdate accretion. Both cratons contain significant concentrations of gold and support thriving gold-mining industries. The most prominent difference between the cratons lies in the nature of the granitoid rocks. The Superior Province is dominated by tonalite and granodiorite whereas the Yilgarn Craton largely consists of granite. This applies to granitoid rocks of all ages in each craton. Granite studies form a major part of this special volume of Precambrian Research." @default.
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- W2052490003 date "1997-05-01" @default.
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- W2052490003 title "Preface: Archaean geology of the Eastern Goldfields of Western Australia — regional overview" @default.
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