Late Quaternary characteristic slip and slip-rate along the Karakax fault (Western Altyn Tagh fault), Tibet
Haibing Li1, Marie-Luce Chevalier2, Dr. Jiawei Pan, PhD3, Zhiming Sun4, Jerome van der Woerd5, Dongliang Liu1 and Jialiang Si6, (1)Key Laboratory of Continental Dynamics, Ministry of Natural Resources, Beijing, China, (2)State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, (3)Chinese Academy of Geological Sciences, Institute of Geology, Beijing, China, (4)Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Resources, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China, (5)University of Strasbourg, Institut Terre et Environnement de Strasbourg, UMR 7063 CNRS, Strasbourg Cedex, France, (6)State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, Beijing, China
