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一、阿尔卑斯地质学的形成格拉鲁斯推复体的发现出露在林特河谷东侧的维尔卡诺岩层一直延伸到山脊附近。维尔卡诺岩层广泛地分布在原来与瑞士接壤的奥地利契洛尔地区,在这里其下部层位是巨厚的三叠纪白云岩等,与三叠纪海相沉积层不同,它的二叠纪陆相岩层的层序已经查明。维尔卡诺岩层具有红色或绿色的特殊岩性,即使从远处,也不会看错。伊塞尔(A.Eseher von Linth,1807—1872)指出,
I. THE FORMATION OF THE ALPINE GEOLOGY The discovery of the Glarus rupture body The Verkano rock formation exposed to the east of the Lint River has been extended to near the ridges. The Vercanano formations are widely distributed in the area of Chilol, Austria, which was originally bordered by Switzerland, where the lower strata are thick Triassic dolostones. Unlike Triassic marine sediments, the Permian The sequence of the Jilu phase strata has been identified. Vercano rock formations have a special lithology of red or green and will not be mistaken even from a distance. According to A. Eherher von Linth (1807-1872)