《Table 3 Palaeostress results.The following information is given for each data site:label used in th

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

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The nine stratigraphic profiles studied in the northern Teruel Basin have been correlated and thereafter projected into two W-E sections，corresponding to the northern（Villalba Alta）and southern（Orrios）sectors of the study area，respectively（Figs.2 and 3）.Detrital deposits crop out in the eastern part of the studied area（e.g.，profiles 4，5，and 6），while carbonates increase westwards（profiles 7 and 8）；in any case，in some profiles（e.g.，1 and 8）both kinds of deposits are present（Fig.3）.Five mappable lithofacies associations，representing sedimentation in a specific sedimentary subenvironment，have been distinguished:Conglomerate（C），Conglomerate and sandstone（CS），Conglomerate and mudstone（CM），Mudstone（M），and Limestone and marl（LM）.The main features of each lithofacies association（lithology and texture，stratal geometry，sedimentary structures）as well as the inferred sedimentary processes and subenvironments are summarised in Table 1 and Fig.4.