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Determining the Age of Terrace Formation Using Luminescence Dating—A Case of the Yellow River Terraces in the Baode Area China

机译:利用发光测年确定梯田形成的年龄-以中国保德黄河梯田为例

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摘要

Dating fluvial terraces has long been a challenge for geologists and geomorphologists, because terrace straths and treads are not usually directly dated. In this study, the formation ages of the Yellow River terraces in the Baode area in China were determined by dating fluvial deposits overlying bedrock straths using optically stimulated luminescence (OSL) dating techniques. Seven terraces (from the lowest terrace T1 to the highest terrace T7) in the study area were recognized, and they are characterized by thick fluvial terrace deposits overlaid by loess sediments. Twenty-five samples from nine terrace sections were dated to about 2–200 ka. The OSL ages (120–190 ka) of the fluvial samples from higher terraces (T3–T6) seem to be reliable based on their luminescence properties and stratigraphic consistency, but the geomorphologic and stratigraphic evidence show that these ages should be underestimated, because they are generally similar to those of the samples from the lower terrace (T2). The formation ages of the terrace straths and treads for the T1 terrace were deduced to be about 44 ka and 36 ka, respectively, based on the deposition rates of the fluvial terrace deposits, and the T2 terrace has the same strath and tread formation age of about 135 ka. The incision rate was calculated to be about 0.35 mm/ka for the past 135 ka, and the uplift rate pattern suggests that the Ordos Plateau behaves as a rigid block. Based on our previous investigations on the Yellow River terraces and the results in this study, we consider that the formation ages of terrace straths and treads calculated using deposition rates of terrace fluvial sediments can overcome problems associated with age underestimation or overestimation of strath or fill terraces based on the single age of one fluvial terrace sample. The implication is that, for accurate dating of terrace formation, terrace sections should be systematically sampled and dated.
机译:长期以来,对河流阶地进行测距一直是地质学家和地貌学家的一项挑战,因为阶地地层和地坪通常不直接标明日期。在这项研究中,中国保德地区黄河阶地的形成年龄是通过使用光学激发发光(OSL)测年技术对河床沉积物覆盖在基岩层之上进行测年来确定的。研究区域中识别出七个阶地(从最低阶地T1到最高阶地T7),它们的特征是由黄土沉积物覆盖的浓厚河床阶地沉积物。来自9个阶地剖面的25个样品的年代约为2–200 ka。基于高阶阶地(T3–T6)的河流样品的OSL年龄(120–190 ka)似乎是可靠的,基于它们的发光特性和地层一致性,但是地貌和地层证据表明这些年龄应被低估,因为它们通常与下平台(T2)的样本相似。根据河床阶地沉积物的沉积速率,推算出T1阶地阶地层地层和胎面的形成年龄分别约为44 ka和36 ka,而T2阶地具有相同的地层和地层形成年龄。约135 ka。对于过去的135 ka,计算的切入速率约为0.35 mm / ka,并且上升速率模式表明鄂尔多斯高原表现为刚性块。根据我们之前对黄河阶地的调查和本研究的结果,我们认为,利用阶地河流沉积物的沉积速率计算的阶地河层和阶地的形成年龄可以克服与年龄低估或过高估测阶地或填充阶地有关的问题。基于一个河流阶地样本的单身年龄。暗示是,为了准确地定阶的阶地,阶地应该被系统地采样和标明日期。

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