Structural Evolution of a 1.6 Ga Orogeny Related to the Final Assembly of the Supercontinent Nuna: Coupling of Episodic and Progressive Deformation-Reference-Cited by-同舟云学术

Structural Evolution of a 1.6 Ga Orogeny Related to the Final Assembly of the Supercontinent Nuna: Coupling of Episodic and Progressive Deformation

Published:2020-10 Issue:10 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Volante S.¹²³^ORCID,Collins W. J.¹^ORCID,Pourteau A.¹,Li Z.‐X.¹^ORCID,Li J.¹^ORCID,Nordsvan A. R.¹⁴

Affiliation:

1. Earth‐Dynamics Research Group, Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences Curtin University Perth Western Australia Australia

2. Institute of Geology, Mineralogy and Geophysics, Ruhr‐Universität Bochum Bochum Germany

3. ISOTOPIA lab, School of Earth, Atmosphere and Environment Monash University Clayton Victoria Australia

4. Department of Earth Sciences University of Hong Kong Hong Kong

Funder

Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006162

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3. Geochemical, Sm–Nd isotopic characteristics and petrogenesis of Paleoproterozoic mafic rocks from the Georgetown Inlier, north Queensland: Implications for relationship with the Broken Hill and Mount Isa Eastern Succession

4. Progressive deformation and reorientation of fold axes in a ductile mylonite zone: the woodroffe thrust

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