Zircons from the Wambidgee Serpentinite Belt, southern Lachlan Orogen: evidence for oceanic crust at the Cambrian–Ordovician boundary-Reference-Cited by-同舟云学术

Zircons from the Wambidgee Serpentinite Belt, southern Lachlan Orogen: evidence for oceanic crust at the Cambrian–Ordovician boundary

Published:2021-10-18 Issue: Volume: Page:1-13
ISSN:0812-0099
Container-title:Australian Journal of Earth Sciences
language:en
Short-container-title:Australian Journal of Earth Sciences

Author:

Belousova E. A.¹²^ORCID,Graham I. T.³^ORCID,Glen R. A.¹^ORCID,Griffin W. L.¹^ORCID,Martin L.⁴^ORCID

Affiliation:

1. ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC National Key Centre, Department of Earth and Environmental Sciences, Macquarie University, Sydney, Australia

2. Department of Resources, Geological Survey of Queensland, Brisbane, Australia

3. Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, University of NSW, Sydney, Australia

4. Centre for Microscopy Characterisation and Analysis, The University of Western Australia, Crawley, Australia

Funder

Australian Research Council Grant

Publisher

Informa UK Limited

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Link

https://www.tandfonline.com/doi/pdf/10.1080/08120099.2021.1981441

Reference75 articles.

1. Age profile of ophiolitic rocks across the Late Palaeozoic New England Orogen, New South Wales: Implications for tectonic models

2. Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons

3. Correction of common lead in U–Pb analyses that do not report 204Pb

4. Field and geochemical characteristics of the Coolac Ophiolite suite and its possible origin in a marginal sea

5. Ashley, P. M., Chenhall, B. E., Cremer, P. L., Irving, A. J. (1971). The geology of the Coolac Serpentinite and adjacent rocks east of Tumut, New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 104, 11–29.

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