Terrane and core complex architecture of the Otago Schist in the Dunstan and Cairnmuir Mountains, New Zealand, from U-Pb and (U-Th)/He zircon dating
Author:
Affiliation:
1. GNS Science, Dunedin, New Zealand
2. Central Washington University, Ellensburg, WA, USA
3. Colorado School of Mines, Golden, CO, USA
4. University of Texas, Austin, TX, USA
Funder
Central Washington University
New Zealand Ministry of Business Innovation and Employment’s Strategic Science Investment Fund
Publisher
Informa UK Limited
Subject
Earth and Planetary Sciences (miscellaneous),Geology,Geophysics
Link
https://www.tandfonline.com/doi/pdf/10.1080/00288306.2023.2176892
Reference76 articles.
1. Tracing the Caples Terrane through New Zealand using detrital zircon age patterns and radiogenic isotope signatures
2. The mid-Cretaceous transition from basement to cover within sedimentary rocks in eastern New Zealand: evidence from detrital zircon age patterns
3. An Australian provenance for the eastern Otago Schist protolith, South Island, New Zealand: evidence from detrital zircon age patterns and implications for the origin of its gold
4. Detrital zircon age studies of Haast Schist in western Otago and Marlborough, New Zealand: constraints on their protolith age, terrane ancestry and Au–W mineralisation
5. Potassium-argon age studies of a low-grade, progressively metamorphosed greywacke sequence, Dansey Pass, South Island, New Zealand
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