Diapir versus along-channel ascent of crustal material during plate convergence: constrained by the thermal structure of subduction zones
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W[2017AGUFM.V24B..03L]
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Key Laboratory of Computational Geodynamics, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, China Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
Key Laboratory of Computational Geodynamics, College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, China