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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Hydrodynamically driven patterns of recent sedimentation in the shelf and upper slope off Southeast Brazil
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Hydrodynamically driven patterns of recent sedimentation in the shelf and upper slope off Southeast Brazil

机译:巴西东南部陆架和上斜坡近期沉积的水动力驱动模式

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Sedimentological parameters of 206 box-core tops and 387 van Veen grab samples were analysed so as to understand the distribution, source and sedimentation rates in the shelf and upper slope of the southern Southeastern Brazilian margin. Most of the parameters (bulk organic matter constituents, delta(13)C, and epsilonNd) can be grouped on northern and southern sectors, separated by a sharp boundary. This suggests that sediment sources and sedimentary processes are different in both regions.The southern sector of the study area is more influenced by cold waters coming from the southern portion of the South American shelf and the organic fraction revealed an important role played by the primary productivity in the sedimentation. Also, epsilonNd values indicate that part of the inorganic fraction of the southern sector sediments are allochtonous, probably coming from younger rocks of the Andean chain probably reaching the shelf through the La Plata river runoff.In the northern part of the study area the sedimentation is controlled almost exclusively by the meandering of Brazil Current. Compositional and isotope bulk organic parameters showed a more complex mixing of terrigenous and pelagic fractions. Also, epsilonNd values are associated with the precambrian rocks of the Brazilian shield. The whole area exhibits sedimentation rates, varying from 5 to 660 mm kyr(-1). (C) 2004 Elsevier Ltd. All rights reserved.
机译:分析了206个箱芯顶和387个van Veen采集样品的沉积学参数,以了解巴西东南部南部陆架和上坡的分布,来源和沉积速率。大部分参数(大块有机物成分,delta(13)C和epsilonNd)可以分为北部和南部两部分,并由尖锐的边界隔开。这表明这两个地区的沉积物来源和沉积过程是不同的。研究区的南部受南美洲大陆架南部的冷水影响更大,有机部分显示了初级生产力的重要作用。在沉淀中。同样,ε值表明南部部分沉积物中的无机部分是异源的,可能来自安第斯链的年轻岩石,可能通过拉普拉塔河径流到达陆架。在研究区域的北部,沉积是几乎完全由“巴西流”的蜿蜒控制。组成和同位素本体有机参数显示陆源和浮游组分的混合更为复杂。而且,ε值与巴西盾的前寒武纪岩石有关。整个区域的沉积速率介于5至660 mm kyr(-1)之间。 (C)2004 Elsevier Ltd.保留所有权利。

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