• WU Weiwei

  WU Weiwei

  1 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 2 School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
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• YANG Jingsui

  YANG Jingsui

  1 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 2 School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
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• MA Changqian

  MA Changqian

  2 School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
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• MILUSHI Ibrahim

  MILUSHI Ibrahim

  3 Department of Geoscience & Geoenvironment, Energy, Water & Environment, Polytechnic University of Tirana, Tirana 1000, Albania
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• LIAN Dongyang

  LIAN Dongyang

  1 CARMA, State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 2 School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
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• TIAN Yazhou

  TIAN Yazhou

  4 College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China
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We thank the Polytech University of Tirana, Albania and other Albania geologists for the assistance in the field work. We thank He Rong for the assistance in the EPMA analyses and the China National Research Center for the geochemical analyses. We would also like to thank Prof. David G.Gee and Prof. Julian A.Pearce for their valuable suggestions in modifying this manuscript. This research was funded by grants from the International Geoscicence Programme (IGCP 649, 2015–2020), the National Natural Science Foundation of China (41541017, 41641015),the Ministry of Science and Technology of China (2014DFR21270), China Geological Survey (12120115026801, 12120115027201, 201511022, DD20160023-01) and the Fund from the State Key Laboratory of Continental Tectonics and Dynamics (Z1301– a20 and K201502).