CENOZOIC EVOLUTION OF THE NULLARBOR PLAIN PALEOKARST, SOUTHERN AUSTRALIA
The Nullarbor Plain in southern Australia is an uplifted succession of Cenozoic marine carbonates whose surface has been exposed for ~14 m.y. This succession of limestones, particularly in the surfical middle Miocene Nullarbor Limestone, hosts a complex and prolonged record of meteoric diagenesis. A...
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| Language: | en en |
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2012
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| Online Access: | http://hdl.handle.net/1974/7319 |