| 
							
      					 | 
  					 
  					
    					 | 
   					 
   										
    					| Corrigendum to "Grain-size and compositional variability of Yarlung Tsangpo sand (Xigaze transect, south Tibet): Implications for sediment mixing by fluvial and aeolian processes" [Journal of Palaeogeography 12 (2) (2023) 195-210] | 
  					 
  					  										
						| Wen Laia, Wen-Dong Liangb, Xiu-Mian Huc,*, Eduardo Garzantid, Hua-Yu Lua, Xiao-Long Dongc | 
					 
															
						aFrontiers Science Center for Critical Earth Material Cycling, School of Geography and Ocean Science, Nanjing University, Nanjing 210023, Jiangsu Province, China;  bState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan Province, China;  cState Key Laboratory of Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, Jiangsu Province, China;  dDepartment of Earth and Environmental Sciences, Università di Milano-Bicocca, Milano 20126, Italy | 
					 
										
						 | 
					 
				 
				
				
					
						
							
								
									
										
											
                        					 
												
													
													    | 
													    	
														 | 
													 
																										
													
														
															
													
													    | 
													     		                            						                            																	     | 
														 
														
														
															| 
															    															    															    															 | 
														 
														 																											    														
															| 
																Corresponding Authors:
																*E-mail address: huxm@nju.edu.cn (X.-M. Hu).   
																													     		
													     	 | 
														 
																																												 
															 | 
															
																
															 | 
													    	
															 | 
																
															
														 
														
													 
													
												 
												
												
												
											
											 
											
											 
										 
									 | 
								 
							 
						 | 
					 
				 
			
		 |