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- W2186405151 abstract "INTRODUCTION The Girilambone Terrain lies between Cobar, Nyngan, Bourke and Nymagee in the western Lachlan Orogen of eastern Australia. This Terrain abuts the Palaeozoic Thomson Orogen to the north and is onlapped by the Mesozoic Surat Basin to the east and north. The Girilambone Terrain is underlain by Cambro-Ordovician Girilambone Group basement rocks with some in-faulted slices of probable Latest Silurian to Early Devonian rocks, perhaps equivalent to the Cobar Supergroup, and some Late Devonian outliers or down-faulted blocks. Granite intrusions, especially in the north, a number of Alaskan-type mafic-ultramafic complexes in the south-east and Miocene leucitites in the central and northern areas intrude and/or overlie this terrain. The Girilambone-Cobar-Nymagee region is one of the richest mineral provinces in New South Wales. Major deposits occur in the Cobar Basin, around Girilambone and at Canbelego and Nymagee, however, exploration has been hampered by the extensive regolith cover as well as poor knowledge of the underlying geology. Much of the area remains to be explored in detail using modern exploration methods." @default.
- W2186405151 created "2016-06-24" @default.
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- W2186405151 date "2005-01-01" @default.
- W2186405151 modified "2023-09-27" @default.
- W2186405151 title "GIRILAMBONE REGOLITH AND LANDSCAPE EVOLUTION" @default.
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