Oligo-Miocene sea-level variations of a karstic coastal system in the Venetian Prealps (Torricelle di Verona, NE Italy): new data

R. Zorzin, G. Cavallo, A. Parlato, Michele Sommaruga, Fabio Tottola
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Abstract

One of the most important European palaeokarstic complexes lies on the southern edge of the Lessini Veronesi Mountains and in particular in the locality of Torricelle di Verona (Veneto region, NE Italy). This 20 kilometre-long network of ancient karstic caves has only recently been made accessible thanks to the exploitation and use of the sediments sealing it, known as coloring earths (yellow and red). It is an intricate system of dendritic natural tunnels that were hydrologically active in the late Miocene and located near the coastline or in direct communication with the sea. Currently few cavities are accessible. The analysis and comparison of the topographic and geomorphic data of the palaeokarstic cavities of the Torricelle allowed the reconstruction of the coastline of the ancient sea of Tethys just before its disappearance.
意大利东北部威尼斯普里阿尔卑斯山脉(Torricelle di Verona)喀斯特海岸系统的渐新世-中新世海平面变化:新资料
欧洲最重要的古岩溶复合体之一位于Lessini Veronesi山脉的南部边缘,特别是在Torricelle di Verona(意大利东北部威尼托地区)。这个长达20公里的古代岩溶洞穴网络直到最近才得以进入,这要归功于对封闭它的沉积物的开采和利用,这种沉积物被称为着色土(黄色和红色)。这是一个复杂的枝状天然隧道系统,在中新世晚期水文活跃,位于海岸线附近或直接与海洋相连。目前很少有可以进入的蛀牙。通过对托里塞勒古岩溶洞穴的地形和地貌数据的分析和比较,可以重建古特提斯海消失前的海岸线。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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