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机译:上次冰川期后,新西兰北岛无冰川的Waipoaa流域的最大河流切口和沉积物产生
Landcare Research, Gisbome 4040, New Zealand,P.O. Box 445, Gisborne 4040, New Zealand;
Landcare Research, Palmerston North 4442, New Zealand;
Institute of Natural Resources, College of Sciences, Massey University, Palmerston North, New Zealand;
Geological and Nuclear Sciences, Wellington, New Zealand;
University of Canterbury, Christchurch, New Zealand;
Geological and Nuclear Sciences, Wellington, New Zealand;
Post-LGM; Onshore fluvial incision; Sediment generation; Landscape response; Hikurangi Margin;
机译:来自新西兰北岛希库朗伊边缘的非冰川Waipaoa和Waimata流域的最后一次冰川聚集和冰川后沉积物的产生
机译:新西兰北岛东海岸怀波阿集水区的坡度对气候调节河道切口的响应
机译:河流网络中的拐点引发和分布:新西兰北岛怀波阿河的236个瀑布
机译:沟壑擦干和沉积物Laaad:Waipaoa,Wawau和Uawa Rivers,Eastern北岛,新西兰
机译:上次冰川最大景观演变,美国三娟山河流河流域,美国
机译:新西兰最后一次冰川最大爆发的早期兴衰
机译:新西兰北岛怀波阿集水区小型降雨汇流的当代泥沙输送比受降雨的影响