首页> 外文期刊>Sedimentology: Journal of the International Association of Sedimentologists >Unit bar architecture in a highly-variable fluvial discharge regime: Examples from the Burdekin River, Australia
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Unit bar architecture in a highly-variable fluvial discharge regime: Examples from the Burdekin River, Australia

机译:单位栏架构在高度可变的河流排放制度:来自Burdekin River,澳大利亚的例子

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摘要

Unit bars are relatively large bedforms that develop in rivers over a wide range of climatic regimes. Unit bars formed within the highly-variable discharge Burdekin River in Queensland, Australia, were examined over three field campaigns between 2015 and 2017. These bars had complex internal structures, dominated by co-sets of cross-stratified and planar-stratified sets. The cross-stratified sets tended to down-climb. The development of complex internal structures was primarily a result of three processes: (i) superimposed bedforms reworking the unit bar avalanche face; (ii) variable discharge triggering reactivation surfaces; and (iii) changes in bar growth direction induced by stage change. Internal structures varied along the length and across the width of unit bars. For the former, down-climbing cross-stratified sets tended to pass into single planar cross-stratified deposits at the downstream end of emergent bars; such variation related to changes in fluvial conditions whilst bars were active. A hierarchy of six categories of fluvial unsteadiness is proposed, with these discussed in relation to their effects on unit bar (and dune) internal structure. Across-deposit variation was caused by changes in superimposed bedform and bar character along bar crests; such changes related to the three-dimensionality of the channel and bar geometry when bars were active. Variation in internal structure is likely to be more pronounced in unit bar deposits than in smaller bedform (for example, dune) deposits formed in the same river. This is because smaller bedforms are more easily washed out or modified by changing discharge conditions and their smaller dimensions restrict the variation in flow conditions that occur over their width. In regimes where unit bar deposits are well-preserved, their architectural variability is a potential aid to their identification. This complex architecture also allows greater resolution in interpreting the conditions before and during bar initiation and development.
机译:单位杆是相对较大的床形,在广泛的气候制度范围内开发河流。在澳大利亚昆士兰州昆士兰州的高度可变排放Burdekin河内形成的单位酒吧在2015年和2017年之间进行了三次野外活动。这些酒吧具有复杂的内部结构,由共分层和平面分层集合主导。交叉分层套装倾向于爬升。复杂的内部结构的发展主要是三个过程的结果:(i)叠加床形式重新加工单位杆雪崩面; (ii)可变放电触发再活化表面; (iii)阶段变化引起的酒吧生长方向的变化。内部结构沿着长度和单元杆的宽度变化。对于前者,攀爬的交叉分层套装倾向于在紧急条的下游端进入单个平面的交叉分层沉积物;与猪条件的变化有关的这种变异,而虽然条是活性的。提出了六种类别的河流不稳定的层次,这些层次有关它们对单位杆(和沙丘)内部结构的影响。倒闭变化是由沿着条形冠的叠加床形和条形的变化引起的;当条形为激活时,与频道和条形几何的三维关系相关的这种变化。内部结构的变化可能在单位杆沉积物中更加明显,而不是在同一条河流中形成的较小榫轮(例如,沙丘)沉积物。这是因为通过改变放电条件并且较小的尺寸更换较小的床单或通过改变较小的尺寸限制它们在其宽度上发生的流动条件的变化。在单位酒吧沉积物被保存完全的制度中,它们的架构变异性是对其识别的潜在援助。这种复杂的架构还允许更大的分辨率来解释Bar启动和开发前和在栏之前和开发期间的条件。

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