{"refrec":{"BRefID":252924,"RR":"<b>Yokokawa, M.; Kishi, M.; Masuda, F.; Yamanaka, M.</b> (1995). Climbing ripples recording the change of tidal current condition in the middle Pleistocene Shimosa Group, Japan, <b><i>in</i></b>: Flemming, B.W. <i>et al.</i> (Ed.) <i>Tidal Signatures in Modern and Ancient Sediments. Special Publication of the International Association of Sedimentologists,</i> 24: pp. 301-311","BEntID":244738,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Flemming, B.W. <i>et al.</i> <i>Tidal Signatures in Modern and Ancient Sediments. Special Publication of the International Association of Sedimentologists,</i> 24: pp. 301-311","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Yokokawa, M.; Kishi, M.; Masuda, F.; Yamanaka, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Yokokawa, M. <i>et al.</i>","Englishabstract":"A lenticular sand body in the middle Pleistocene Shimosa Group in Japan, dominated by climbing ripple cross-lamination, is interpreted here as an estuarine or lagoonal deposit that accumulated under tidal influences. Based on the systematic change of sand-layer thickness in the alternation of sand and mud layers, two sets of four neap-spring tidal cycles are reconstructed from tidal flat deposits that occur just above the climbing-rippled sand. The climbing ripple cross-laminae occur as four different types which signify variable current velocities and sediment supply. lsochrons can be drawn through the climbing-rippled sand along individual bedding surfaces on detailed tracings of the climbing ripple cross-laminae. The dominant types of climbing ripple cross-lamination vary along each isochron. Cyclic variations in current velocity during a single tidal cycle are demonstrated from the vertical evolution in the types of climbing ripple cross-lamination. 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