This article was downloaded by: [Queensland University of Technology] On: 29 March 2015, At: 14:27 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Click for updates Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia Publication details, including instructions for authors and subscription information: http:/ / www.tandfonline.com/ loi/ taje20 A new period of volcanogenic massive sulfide formation in the Yilgarn: a volcanological study of the ca 2.76 Ga Hollandaire VMS deposit, Yilgarn Craton, Western Australia P . C. Hayman a , S. E. Hull a , R. A. F. Cas a , E. Summerhayes b , Y. Amelin c , T. J. Ivanic d & D. Price e a Earth Atmosphere and Environment, Monash University, Clayton, Victoria 3800, Australia b Silver Lake Resources, Suite 4, Level 3, South Shore Centre, 85 South Perth Esplanade, South Perth, WA 6151, Australia c The Australian National University, Canberra, ACT 0200, Australia d Geological Survey of Western Australia, Mineral House, 100 Plain Street, East Perth, WA 6004, Australia e Exploration Manager at Savannah Resources, 2nd Floor, 18 Pall Mall, London SW1Y 5LU, UK Published online: 24 Mar 2015. To cite this article: P . C. Hayman, S. E. Hull, R. A. F. Cas, E. Summerhayes, Y. Amelin, T. J. Ivanic & D. Price (2015) A new period of volcanogenic massive sulfide formation in the Yilgarn: a volcanological study of the ca 2.76 Ga Hollandaire VMS deposit, Yilgarn Craton, Western Australia, Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia, 62:2, 189-210, DOI: 10. 1080/ 08120099. 2015. 1011399 To link to this article: ht t p:/ / dx.doi.org/ 10.1080/ 08120099.2015.1011399 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. This article may be used for research, teaching, and private study purposes. Any substantial or systematic reproduction, redistribution, reselling, loan, sub-licensing, systematic supply, or distribution in any