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Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Large earthquake recurrence on the southern Willunga Fault, South Australia
The presence of Pliocene marine sediments in the Myponga and Meadows basins within the Mt Lofty Ranges south of Adelaide is testament to over 200 m of tectonic uplift... -
Spatial variations in lead isotopes, Tasman Element, eastern Australia
Lead isotope data from ore deposits and mineral occurrences in the Tasman Element of eastern Australia have been used to construct isotopic maps of this region. These maps... -
Crustal structure across the Lord Howe Rise, northern Zealandia, and rifting...
During the Late Cretaceous, the fragmentation of eastern Gondwana led to the formation of the narrow eastern Australian margin and the wide Lord Howe Rise during the opening of... -
Delayed subsidence after rifting and a record of breakup for northwestern Zealandia
Continental rifting and breakup of eastern Gondwana during the Cretaceous separated northern Zealandia from eastern Australia, but the processes leading to this highly-extended... -
The Paleoproterozoic Trans-Australian Orogen: its magmatic and...
The 2.1─1.79 Ga Trans-Australian and Canadian Trans-Hudson orogens preserve a common record of Himalayan-scale orogenesis and voluminous Cordilleran-style magmatism behind which...