Provenance changes and movement on the Alpine Fault indicated by heavy minerals from Cretaceous-Cenozoic sediments in south Westland
Author:
Publisher
Informa UK Limited
Subject
Multidisciplinary
Link
http://www.tandfonline.com/doi/pdf/10.1080/03036758.1991.10431403
Reference28 articles.
1. Inferred uplift rates from raised marine surfaces, southern Fiordland, New Zealand
2. A study of detrital heavy minerals in the Taramakau catchment
3. Heavy minerals from Southland
4. The Dun Mountain ophiolite belt, New Zealand, its tectonic setting, constitution, and origin, with special reference to the southern portion
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1. Regional geological framework of South Island, New Zealand, and its significance for understanding the active plate boundary;A Continental Plate Boundary: Tectonics at South Island, New Zealand;2007
2. Chapter 22 Sediment Trails in Tectonically Active Islands: Heavy Minerals in Use in New Zealand;Developments in Sedimentology;2007
3. PHYLOGEOGRAPHY OF THE NEW ZEALAND CICADA MAORICICADA CAMPBELLI BASED ON MITOCHONDRIAL DNA SEQUENCES: ANCIENT CLADES ASSOCIATED WITH CENOZOIC ENVIRONMENTAL CHANGE;Evolution;2001-07
4. Torlesse greywacke and Haast Schist source for Pliocene conglomerates near Reefton, New Zealand;New Zealand Journal of Geology and Geophysics;2001-03
5. Tectonic reconstructions of New Zealand: 40 Ma to the Present;New Zealand Journal of Geology and Geophysics;2000-12
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