《Table 1 Lithofacies associations distinguished for the Pliocene-Pleistocene record in the northern

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《"Alluvial sedimentation and tectonostratigraphic evolution in a narrow extensional zigzag basin margin (northern Teruel Basin, Spain)"》

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Two sets of alluvial fans can be distinguished considering the radius length and sourcing areas（Figs.5 and 6）.Small alluvial fans（SAF），fed by the footwall of NNW-SSE faults，are up to 5 km long and show westwarddirected palaeocurrents，whereas very small alluvial fans（VSAF），shorter than 1 km，are mainly northwestdirected and fed by NNE-SSW faults.Basinwards，lithofacies LM（Table 1，Fig.4）represents shallow，low-energy，fresh-water lakes and palustrine fringes.Although lakes were dominated by carbonate precipitation，they also received detrital supplies from the alluvial fans.