Geochemistry, Geophysics, Geosystems Supporting Information for Receiver function imaging of the mantle transition zone beneath the South China Block Haibo Huanga, Nicola Tosib,c, Sung-Joon Changd, Shaohong Xiaa, Xuelin Qiua a b c d CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China; Department of Astronomy and Astrophysics, Technische Universität Berlin, Hardenberg Strasse 36, 10623, Berlin, Germany; Department of Planetary Physics, German Aerospace Center (DLR), Rutherford Strasse 2, 12489, Berlin, Germany; Division of Geology and Geophysics, Kangwon National University, Gangwondaehak-gil 1, Chuncheon-si, Gangwon-do, 200-701, South Korea Contents of this file Figure S1 Data Set S1 Additional Supporting Information (Files uploaded separately) Data Set S1 contains the 4172 high-quality receiver functions we used for phaseweighted common conversion points stacking. Introduction This supporting information contains maps of the transition zone thickness and of the topography of the 410 km and 660 km discontinuities for different 3D and 1D models (Figure S1). It also provides the receiver functions used for stacking that can be processed by SAC (Seismic Analysis Code). 1 Figure S1. Maps of the transition zone thickness (top), and of the topography of the 410 (bottom) and 660 (middle) for different 3D and 1D models. The transition zone thickness is calculated by subtracting the depth of the 660 from that of the 410. The average values are marked on the top left corner of the maps. The color scales denote variations with respect to the average values. 1 Data Set S1. Receiver functions used for phase-weighted common conversion points stacking. Files are named, e.g. as “H30_2001010161347_GD_SHG”, where H30 means that the waveforms include 30 s before the theoretical P arrival time; 2001010161347 is the time of the teleseismic events; GD is the name of the seismic network while SHG is the station name. 1