Tectonics control on Quaternary sedimentary processes and basin infill from the coastal area to the basin plain: examples from the Capo d'Orlando Basin (Southeastern Tyrrhenian Sea)

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
F. Gamberi
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引用次数: 2

Abstract

Tectonic activity can affect every single segment of a sedimentary system and the various environments within a basin react in specific ways to tectonic forcing. However, the outcomes of tectonic activity on one environment have important consequences on the sedimentary processes in adjacent ones. In this paper, I evaluate the relationships between tectonic activity and sedimentary processes in several distinct environments, and in different times within the last sea- level cycle, in the submarine part of a single sedimentary system: the Capo d'Orlando Basin. The study area is located in the southeastern Tyrrhenian Sea along the northern Sicilian margin and is affected by active tectonics. A multibeam bathymetric coverage, chirp and regional sparker profiles are available over the study area. In the shelf, the Caronia Horst controls the thickness of the high stand systems tract and the character and the preservation potential of the coastal deposits of the transgressive systems tract. Coastal physiography, due to differential vertical movements, affects offshore current strength and pattern of sediment transport, causing the sand-mud line to move offshore. In the upper slope, tilting increases sediment instability and the accumulation of landslide deposits. Uplift, responsible for the local shallower depth of the shelf edge, favoured the connection between canyon heads and river mouths during the last sea-level low stand. More importantly, some of the canyon heads are still close to the coast and can receive sediment from rivers or offshore currents even during the present-day high stand. The Naso and the Calava Channels have fault-controlled courses and an asymmetric profile, which controls the location of overbank flows, sediment failures and landslide deposition. In the basin plain, the continued activity of the major faults has created subtle topography and the turbidite lobes do not present a compensational stacking pattern but remain fixed in fault-controlled lows; differential compaction in the separate fault blocks also contribute to differences in turbidite thickness. Landslides are present at the base of the fault-controlled basin-bounding escarpments and punctuate the otherwise turbidite-dominated succession. The analysis of the Capo d'Orlando Basin illustrates the range of effects that tectonic structures have on sedimentary processes going from the continental shelf to the basin plain. More importantly, although in a qualitative way, this research shows how the tectonic influence on up-dip processes is also responsible for the nature of the depositional record in the deeper part of the basin.
从沿海地区到盆地平原的第四纪沉积过程和盆地填充的构造控制:以Capo d‘Orlando盆地为例(第勒尼安海东南部)
构造活动可以影响沉积系统的每一个环节,盆地内的各种环境以特定的方式对构造作用力作出反应。然而,构造活动对一个环境的影响对相邻环境的沉积过程具有重要影响。在这篇论文中,我评估了在几个不同的环境中,在上一个海平面周期的不同时期,在单一沉积系统的海底部分,即Capo d‘Orlando盆地,构造活动和沉积过程之间的关系。研究区域位于西西里岛北部边缘的第勒尼安海东南部,受活动构造影响。研究区域内有多波束测深覆盖、线性调频和区域sparker剖面。在陆架中,Caronia Horst控制着高位体系域的厚度以及海侵体系域海岸沉积物的特征和保存潜力。由于不同的垂直运动,海岸地貌影响了近海洋流强度和沉积物输送模式,导致沙泥线向近海移动。在上斜坡,倾斜增加了沉积物的不稳定性和滑坡沉积物的堆积。隆起是陆架边缘局部较浅深度的原因,有利于在上一次海平面低水位期间峡谷顶部和河口之间的连接。更重要的是,一些峡谷头仍然靠近海岸,即使在今天的高地,也可以接收来自河流或离岸流的沉积物。纳索河和卡拉瓦河河道具有断层控制河道和不对称剖面,控制着河岸上水流、沉积物破坏和滑坡沉积的位置。在盆地平原,主要断层的持续活动创造了微妙的地形,浊积岩凸角不呈现补偿叠加模式,但仍固定在断层控制的低点;不同断块的差异压实也导致了浊积岩厚度的差异。滑坡出现在断层控制盆地的底部,边界为悬崖,并打断了以浊积岩为主的序列。对Capo d‘Orlando盆地的分析说明了构造结构对从大陆架到盆地平原的沉积过程的影响范围。更重要的是,尽管是定性的,但这项研究表明,构造对上倾过程的影响也是盆地深层沉积记录性质的原因。
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来源期刊
Italian Journal of Geosciences
Italian Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
2.90
自引率
11.10%
发文量
25
审稿时长
>12 weeks
期刊介绍: The Italian Journal of Geosciences (born from the merging of the Bollettino della Società Geologica Italiana and the Bollettino del Servizio Geologico d''Italia) provides an international outlet for the publication of high-quality original research contributions in the broad field of the geosciences. It publishes research papers, special short papers, review papers, discussion-and-replies for their rapid distribution to the international geosciences community. The journal is firstly intended to call attention to the Italian territory and the adjacent areas for the exceptional role they play in the understanding of geological processes, in the development of modern geology and the Earth sciences in general. The main focus of the journal is on the geology of Italy and the surrounding sedimentary basins and landmasses, and on their relationships with the Mediterranean geology and geodynamics. Nevertheless, manuscripts on process-oriented and regional studies concerning any other area of the World are also considered for publication. Papers on structural geology, stratigraphy, sedimentology, basin analysis, paleontology, ecosystems, paleoceanography, paleoclimatology, planetary sciences, geomorphology, volcanology, mineralogy, geochemistry, petrology, geophysics, geodynamics, hydrogeology, geohazards, marine and engineering geology, modelling of geological process, history of geology, the conservation of the geological heritage, and all related applied sciences are welcome.
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