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Continental slope-confined canyons in the Pearl River Mouth Basin in the South China Sea dominated by erosion, 2004-2018

机译:2004年至2018年,南海珠江口盆地的大陆斜坡受限峡谷受侵蚀侵蚀

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Repeat multibeam bathymetric surveys conducted in 2004, 2005 and 2018 show that seven slope-confined canyons on the continental slope of the Pearl River Mouth Basin, South China Sea, were dominated by large volume, widespread erosion. Erosion volumes were up to 3.4 times greater than deposition volumes. Erosion-dominated areas of the canyons are up to 2.3 times greater than areas dominated by deposition. Average rates of erosion (ranging from 0.7 to 0.8 m/yr) were greater than average rates of deposition (ranging from 0.5 to 0.8 m/yr). In plan view, the erosion-dominated zones exhibit two characteristic shapes: (1) linear, found mainly in upper canyon reaches, distributed predominantly along canyon axes and at the base of eastern canyon walls, and; (2) blocky, found mainly in lower canyon reaches, widely distributed along the steep canyon walls and on lower-canyon interfluves. The deposition-dominated zones are scattered along canyon floors and walls. Seismic reflection data show lateral shifts of canyon fill deposits through time, indicative of longer-term eastward canyon migration. The linear erosion-dominated zones may be attributed to erosive turbidity currents triggered by energetic internal solitary waves shoaling on the shelf. The eastward canyon shifts were likely induced by rapid near-bed eastward currents generated mainly by westward propagating powerful internal solitary waves of depression. The widespread erosion in the deeper canyon areas and interfluves is likely a consequence of slope instabilities associated with the presence of gas hydrates. This study indicates that active sedimentary processes can occur in slope-confined canyons even during sea level highstands. Local, site-specific oceanographic and geological features (e.g., internal solitary waves, gas hydrates) can significantly increase sedimentary activity in and around submarine canyons. (C) 2019 Elsevier B.V. All rights reserved.
机译:分别在2004年,2005年和2018年进行的多波束测深调查表明,南海珠江口盆地大陆坡上的七个边坡受限的峡谷以大量的广泛侵蚀为主。侵蚀量高达沉积量的3.4倍。峡谷中以侵蚀为主的区域比沉积为主的区域大2.3倍。平均侵蚀速率(0.7至0.8 m / yr)大于平均沉积速率(0.5至0.8 m / yr)。在平面图中,侵蚀占主导的区域表现出两个特征形状:(1)线性,主要出现在峡谷上段,主要沿峡谷轴线和东部峡谷壁的底部分布;以及(2)块状,主要见于下峡谷,广泛分布于陡峭的峡谷壁和下峡谷的交汇处。沉积为主的区域沿峡谷的底面和墙壁散布。地震反射数据显示,随着时间的推移,峡谷填充物的横向移动表明了长期的东移。线性侵蚀占主导的区域可归因于在架子上潜入的高能量内部孤波触发的侵蚀性浊流。向东的峡谷移动很可能是由快速的近床东流引起的,这主要是由向西传播的强烈的内部孤波产生的。较深的峡谷区域和河道之间的广泛侵蚀很可能是与天然气水合物存在相关的边坡不稳定性的结果。这项研究表明,即使在海平面高处,活跃的沉积过程也可能发生在斜坡限制的峡谷中。特定地点的特定海洋学和地质特征(例如内部孤立波,天然气水合物)可以显着增加海底峡谷内和周围的沉积活动。 (C)2019 Elsevier B.V.保留所有权利。

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