Zircons traced from the 700-500 Ma Transgondwanan Supermountains and the Gamburtsev Subglacial Mountains to the Ordovician Lachlan Orogen, Cretaceous Ceduna Delta, and modern Channel Country, Central-Southern Australia

J. J. Veevers^*, E. A. Belousova, A. Saeed

^*Corresponding author for this work

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

Research output: Contribution to journal › Article › peer-review

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Dating Down Under: Resolving Earth's Crust - Mantle Relationships (MQ)
Belousova, E.
1/05/12 → 30/04/13
Project: Research