首页> 外文期刊>Journal of Maps >The Meso–Cenozoic stratigraphic succession of the Col de Braus area (Maritime Alps, SE France)
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The Meso–Cenozoic stratigraphic succession of the Col de Braus area (Maritime Alps, SE France)

机译:科尔布劳斯地区(法国阿尔卑斯山,法国东南部)的中新生代地层演替

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The 1:10,000 geological map here presented extends over about 32?km~(2) around the Col de Braus pass in the Maritime Alps (SE France). This area has attracted the attention of geologists since the late eighteenth century due to superb exposures of the Jurassic–Cretaceous Proven?al succession, and has become a classic geological locality continuously studied until the present day. In this area, Early Cretaceous synsedimentary tectonics is evidenced by important lateral thickness and facies variations. This sector is presently placed at the western termination of a large structural domain extending from the westernmost Ligurian Alps into the French–Italian Maritime Alps, thus representing a key-area for understanding the structural setting of this part of the Western Alps.
机译:这里呈现的1:10,000地质图围绕着海上阿尔卑斯山(法国东南部)的Col de Braus通行证延伸了约32?km〜(2)。自从18世纪末以来,由于侏罗纪-白垩纪证据演替的大量曝光,该地区引起了地质学家的关注,并且成为了一个不断研究直到今天的经典地质地区。在该地区,重要的侧向厚度和相变证明了早白垩世的沉积构造。该部门目前位于从最西端的利古里亚阿尔卑斯山延伸到法国-意大利海事阿尔卑斯山的大型结构域的西端,因此是理解西阿尔卑斯山这部分结构的关键区域。

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