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MIS 9 to MIS 5 terraces along the Tyrrhenian Sea coast of Latium (central Italy): Assessing interplay between sea-level oscillations and tectonic activity

机译:提滕尼海沿拉提姆海岸(意大利中部)的MIS 9至MIS 5阶地:评估海平面波动与构造活动之间的相互作用

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We present a review of the geomorphology of the Tyrrhenian Sea coast of central Italy integrated by a novel structural-geomorphological study coupled with statistical analysis of topographic culminations and comparison with a Digital Elevation Model, aimed at reconstructing a suite of paleo-surfaces corresponding to remnant portions of marine terraces. We performed geochronological, sedimentological, micromorphological and mineralogical investigations on the deposits forming the different paleo-surfaces between Civitavecchia and Anzio towns, in order to provide chronostratigraphical, paleo-geographical and paleoenvironmental constraints. Using the newly achieved dataset we correlate these paleo-surfaces with the coastal terraces formed during past sea-level highstands, as recognized by previous studies, and we refine their correlation with the Marine Isotope Stage (MIS) timescale.In particular, we have extended our geomorphological analyses landward in the area between the Tiber River mouth and Anzio, in order to include the oldest paleo-surface developed above the deposits of the last large explosive eruption at 365 +/- 4 ka in the Colli Albani Volcanic District. Results of this study allow us to recognize a set of higher paleo-surfaces at elevation ranging 108 thought 71 m a.s.l., which we interpret as one tectonically displaced, widespread coastal terrace originated during the MIS 9.1 highstand. We correlate the previously identified paleo-surfaces of 66-62 m a.s.l. and 56-52 m a.s.l. with the equivalent coastal terraces developed during the sea-level highstands of sub-stages 7.5 and 7.3/7.1. Moreover, based on data from literature on relative elevation of maximum sea level during the highstands of MIS 11 through MIS 5.1, we assess the regional uplift and the concurrent tectonic displacements that have occurred since 900 ka in this area. (C) 2019 Elsevier B.V. All rights reserved.
机译:我们目前对意大利中部第勒尼安海沿岸的地貌进行回顾,该研究是通过新颖的结构-地貌学研究与地形高潮的统计分析以及与数字高程模型的比较相结合,旨在重建一组对应于残余物的古地表海洋阶地的一部分。为了提供年代地层,古地理和古环境的限制,我们对奇维塔韦基亚和安齐奥镇之间形成不同古地表的沉积物进行了地质,沉积,微形态和矿物学研究。正如先前的研究所确认的那样,使用新获得的数据集,我们将这些古地表与过去海平面高位形成的沿海阶地相关联,并完善了它们与海洋同位素阶段(MIS)时间尺度的相关性。我们的地貌分析是在台伯河河口和安齐奥之间的区域内陆上进行的,目的是包括在库里阿尔巴尼火山区最后一次大爆发喷发的沉积物上方365 +/- 4 ka上方形成的最古老的古地表。这项研究的结果使我们能够识别出海拔108到71 m a.s.l.的一组较高的古地表,我们将其解释为一个构造位移,广泛的沿海阶地,发源于MIS 9.1高潮。我们将先前确定的66-62 m a.s.l的古表面关联起来。和56-52 m a.s.l.以及在7.5和7.3 / 7.1子阶段的海平面高位开发的同等沿海阶地。此外,根据有关MIS 11到MIS 5.1的高位期间最大海平面的相对高程的文献数据,我们评估了该地区自900 ka以来发生的区域隆升和同时发生的构造位移。 (C)2019 Elsevier B.V.保留所有权利。

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