Reassessment of continental growth during the accretionary history of the Central Asian Orogenic Belt

Gondwana Research - Tập 25 - Trang 103-125 - 2014
A. Kröner1,2, V. Kovach3, E. Belousova4, E. Hegner5, R. Armstrong6, A. Dolgopolova6, R. Seltmann6, D.V. Alexeiev7, J.E. Hoffmann8, J. Wong9, M. Sun9, K. Cai9, T. Wang10, Y. Tong10, S.A. Wilde11, K.E. Degtyarev7, E. Rytsk3
1Beijing SHRIMP Centre, Chinese Academy of Geological Sciences, Beijing, China
2Department of Geosciences, University of Mainz, Germany
3Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia
4Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia
5Department of Geo- and Environmental Sciences, University of Munich, Germany
6CERCAMS, Department of Earth Sciences, Natural History Museum, London, UK
7Geological Institute, Russian Academy of Sciences, Moscow, Russia
8Department of Geology and Mineralogy, University of Cologne, Germany
9Department of Earth Sciences, the University of Hong Kong, Pokfulam Road, Hong Kong, China
10Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
11Institute for Geoscience Research, Department of Applied Geology, Curtin University of Technology, Perth, WA 6845, Australia

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