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Nathan R. Daczko

Researcher at Macquarie University

Publications -  107
Citations -  2839

Nathan R. Daczko is an academic researcher from Macquarie University. The author has contributed to research in topics: Granulite & Metamorphism. The author has an hindex of 29, co-authored 98 publications receiving 2362 citations. Previous affiliations of Nathan R. Daczko include University of Vermont & University of New England (Australia).

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A cryptic Gondwana-forming orogen located in Antarctica.

TL;DR: The most poorly exposed and least understood Gondwana-forming orogen lies largely hidden beneath ice in East Antarctica as discussed by the authors, suggesting that the Kuunga orogen sutured provinces of broadly Indian versus Australian affinity.
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Cretaceous high‐P granulites at Milford Sound, New Zealand: metamorphic history and emplacement in a convergent margin setting

TL;DR: Granulite facies orthogneiss of the Arthur River Complex (ARC) at Milford Sound, western Fiordland records a complex Early Cretaceous magmatic and orogenic history for the Pacific Gondwana margin that culminated in the emplacement and burial of a dioritic batholith, the Western FIordland Orthognes (WFO) as mentioned in this paper.
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Fingerprinting Proterozoic bedrock in interior Wilkes Land, East Antarctica

TL;DR: These new geological insights into the ice-covered bedrock of Wilkes Land substantially improve correlations of Antarctic and Australian geological elements and provide key constraints on the tectonic architecture of this sector of the East Antarctic Shield and its role in supercontinent reconstructions.
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Decoding near-concordant U–Pb zircon ages spanning several hundred million years: recrystallisation, metamictisation or diffusion?

TL;DR: In situ isotopic (U-Pb, Lu-Hf) and trace element analyses of zircon populations in six samples of the intrusive Mawson Charnockite, east Antarctica, emphasise complex ZIRcon behavior during very high-grade metamorphism.
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Kinematic vorticity and tectonic significance of superposed mylonites in a major lower crustal shear zone, northern Fiordland, New Zealand

TL;DR: In this article, structural, metamorphic, finite strain and kinematic vorticity data from a 4 km-wide, subvertical shear zone in Fiordland, New Zealand reveal a history of deformation reflecting different tectonic regimes.