Evidence for Ordovician subduction-related magmatism in the Truong Son terrane, SE Laos: Implications for Gondwana evolution and porphyry Cu exploration potential in SE Asia

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Funding Acknowledgements

This project would have not been possible without the financial and logistical support of PT (Sole) Company Ltd., with its exploration crews and support staff, namely Fraser Gardiner, providing invaluable in-field assistance. Special thanks are made to William Powell and the team at the ARC CCFS and National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC) at Macquarie University, Australia for their outstanding support. The analytical data were obtained using instrumentation funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners and Macquarie University. This is contribution 858 from the ARC Centre of Excellence for Core to Crust Fluid Systems (http://www.ccfs.mq.edu.au) and 1116 in the GEMOC Key Centre (http://www.gemoc.mq.edu.au). The authors would also like to acknowledge the XRF Facility within the MarkbWainwright Analytical Centre at the University of New South Wales, and the Q-ICP-MS unit in the School of Earth Sciences, University of Melbourne, Australia for their analytical support. And finally, we would also like to thank Ian Metcalfe and Mei-Feng Shi for their helpful reviews which improved the final revised manuscript.