Evidence for Deformation in the Cambrian‐Ordovician Warburton Basin and Implications for the Evolution of the Tasmanides (Eastern Australia)-Reference-Cited by-同舟云学术

Evidence for Deformation in the Cambrian‐Ordovician Warburton Basin and Implications for the Evolution of the Tasmanides (Eastern Australia)

Published:2019-05 Issue:5 Volume:38 Page:1532-1555
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Abdullah Rashed¹^ORCID,Nugroho Rio¹^ORCID,Rosenbaum Gideon¹^ORCID,Doublier Michael P.²^ORCID,Shaanan Uri¹³^ORCID,Zwingmann Horst⁴^ORCID

Affiliation:

1. School of Earth and Environmental Sciences The University of Queensland Brisbane Queensland Australia

2. Geoscience Australia Canberra Australia

3. Institute of Earth Sciences Hebrew University of Jerusalem Jerusalem Israel

4. Division of Earth and Planetary Sciences, Graduate School of Science Kyoto University Kyoto Japan

Funder

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005124

Reference101 articles.

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2. Devonian Crustal Stretching in the Northern Tasmanides (Australia) and Implications for Oroclinal Bending

3. Armistead S. &Fraser G. L.(2015) New SHRIMP U‐Pb zircon ages from the Cuttaburra and F1 prospects southern Thomson Orogen New South WalesRep. 1925124819.

4. A re‐appraisal of the Darling Basin Devonian sequence;Bembrick C.;Geological Survey of New South Wales Quarterly Notes,1997

5. Black L. P.(2006) SHRIMP U‐Pb zircon ages obtained during 2005/06 for NSW Geological Survey projects edited Geological Survey of New South Wales GS 2006/821.

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