Eocene to Miocene Out-of-Sequence Deformation in the Eastern Tibetan Plateau: Insights From Shortening Structures in the Sichuan Basin

Grants

Funding Acknowledgements

Funding for this research was provided by Chinese 1000 Young Talents Program, National Natural Science Foundation of China (NSFC) grant 41772211, U1701641 and the Guangdong Province Introduced Innovative R&D Team (2016ZT06N331). The University of Melbourne thermochronology laboratory receives infrastructure support from the Australian Research Council and the AuScope Program of NCRIS. The authors are grateful to Chuanqing Zhu, Ming Xu, Jianzhong Qin and Tenger for their field assistance, and to Abaz Alimanovic, Brent McInnes and Noreen Evans for technical assistance with (U-Th-Sm)/He dating. Constructive reviews by Bastian Wauschkuhn and Andrew Zuza clarified many points in this article. A more detailed discussion of the analytical methodology can be found in the supporting information (Farley et al., 1996; Galbraith, 2005; Gleadow et al., 2009; House et al., 2000; Jochum et al., 2011; Ketcham et al., 2007). The data for this paper are included in the manuscript and the associated supporting information.