保拉盆地 Amantea 扇(第勒尼安海东南部)一个封闭的深海扇叶中超临界床形的下坡演化

IF 2.7 2区 地球科学 Q1 GEOLOGY
E. Scacchia , R. Tinterri , F. Gamberi
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引用次数: 0

摘要

上层流体床形的沉积学是当前的一个重要研究课题。在现代扇形水系中,被解释为超临界流的沉积物已得到广泛认可,但对其进行复原却极具挑战性。大部分沉积学信息来自河道干流,但超临界床形也经常出现在河道口的下坡。在保拉盆地就发现了这样的环境,那里的侵蚀和沉积循环台阶已在阿曼特扇的沙质海底叶片中成像并得到确认。高分辨率的海底剖面图让人们深入了解了床形的内部结构及其与前缘海脊的关系。这是第一次在两个不同的位置对海底浅滩的超临界床形进行解释:侵蚀性循环台阶的冲刷区和沉积性循环台阶的stoss侧。在冲刷区和山脊脚发现了带有火焰结构的粗粒到中粒的块状砂,这表明沉积物的快速沉降,并经常与水力跃层的出现有关。后者是由地形引起的水力跃升的一个例子,其驱动力是锋面限制。顶部切割出的具有牵引结构的中细砂被解释为与旋回台阶或叠加在旋回台阶表面的小规模反沙丘的台阶侧有关的沉积物。所提供的数据拓宽了人们对浊流与海底地形和斜坡倾角之间相互作用所驱动的一系列过程的认识。认识到地形会影响浊流的密度结构和临界程度,从而影响相对沉积物的形态动力学和面貌,这可能有助于解释沉积物的分布,并改进封闭环境中扇叶的沉积模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Downslope evolution of supercritical bedforms in a confined deep-sea fan lobe, Amantea Fan, Paola Basin (Southeastern Tyrrhenian Sea)

The sedimentology of upper flow regime bedforms represents an important research topic at the present. Deposits interpreted as those of supercritical flows are widely recognized in modern fan systems, but their recovery is challenging. Most of the sedimentological information has come from channel thalwegs but supercritical bedforms are also frequently downslope from the channel mouths. Such an environment has been identified in the Paola basin, where erosive and depositional cyclic steps have been imaged and identified in a sandy submarine lobe of the Amantea Fan. High-resolution sub-bottom profiles provide insight into the bedform internal architecture and their relationships with a frontally-confining ridge. For the first time, supercritical bedforms in a submarine lobe have been interpreted in two distinct positions: in the scour of an erosional cyclic step and in the stoss side of a depositional cyclic step. Coarse to medium-grained massive sand with flame structures, indicating rapid sediment fall-out and frequently associated with the occurrence of hydraulic jumps, has been identified in the scour and at the toe of the ridge. The latter represents an example of topographically induced hydraulic jumps driven by a frontal confinement. Top-cut-out medium to fine sands with tractive structures have been interpreted as the deposits related to the stoss side of a cyclic step or small-scale antidune superimposed on the cyclic step surface. The presented data broaden the understanding of the range of processes that are driven by the interaction between turbidity currents and seafloor topography and the dip of the slope. The recognition that topography influences the density structure and the degree of criticality of the flow and, consequently, the morphodynamics and facies of the relative deposits may help to explain sediment distribution and improve depositional models of fan lobes in confined settings.

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来源期刊
Sedimentary Geology
Sedimentary Geology 地学-地质学
CiteScore
5.10
自引率
7.10%
发文量
133
审稿时长
32 days
期刊介绍: Sedimentary Geology is a journal that rapidly publishes high quality, original research and review papers that cover all aspects of sediments and sedimentary rocks at all spatial and temporal scales. Submitted papers must make a significant contribution to the field of study and must place the research in a broad context, so that it is of interest to the diverse, international readership of the journal. Papers that are largely descriptive in nature, of limited scope or local geographical significance, or based on limited data will not be considered for publication.
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