【作者】Zhenyu Li，Lin Ding，Douwe J.J. van Hinsbergen，Peter C. Lippert，Yahui Yue，Jing Xie，Yaofei Chen，Xudong Guo，Dingding Zhang，Tengge Zhao，Bailing Wu，Hangjun Li，Songlin He
【作者单位】1 State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; 2 Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China; 3 University of Chinese Academy of Sciences (UCAS), Beijing 100049, China; 4 Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands; 5 Department of Geology and Geophysics, The University of Utah, Salt Lake City, 84112, UT, USA; 6 Institute of Science and Technology Strategy, Jiangxi Academy of Sciences, Nanchang 330029, China; 7 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 8 College of Engineering and Technology, Tibet University, Lhasa 850000, China
【摘要】 Paleomagnetic data constrain paleogeographic motion of rocks relative to the Earth's spin axis, which is a sum of plate motion relative to the mantle and true polar wander. Discerning between these effects is challenging for studies aiming to reconst...
