ABSTRACT

The studied area, located in the south-western part of the Gorce Mountains, is built of flysch deposits representing the Krynica and Bystrica Subunits of the Magura Nappe. Here, in the Late Cretaceous–Early Miocene part of the lithostratigraphic succession of the Krynica Subunit, four formations containing several members were distinguished, whereas in the Bystrica Subunit, only one Middle Eocene–Oligocene formation was identified. The Turbacz and Kudłoń Thrust Sheets in the tectonic structure of the Krynica Subunit and the southernmost fragment of the Tobołów Thrust Sheet in the Bystrica Subunit are prominent. Several folds occur in the studied area. Numerous transverse and oblique faults are also present. The result of the present geological investigations in the study area was the creation of a geological map of the Magura Nappe deposits in the Gorce Mountains. In general, a high-resolution digital elevation model contributed significantly to the progress of this geological research.

摘要

研究区位于 Gorce 山脉的西南部，由代表 Magura Nappe 的 Krynica 和 Bystrica 亚基的复理石矿床构成。在这里，在 Krynica 亚基的岩石地层序列的晚白垩世 - 早中新世部分，区分了包含几个成员的四个地层，而在 Bystrica 亚基中，只确定了一个中始新世 - 渐新世地层。Krynica 亚单元构造结构中的 Turbacz 和 Kudłoń 逆冲断层以及 Bystrica 亚单元中 Tobołów 逆断层最南端的碎片是突出的。在研究区域发生了几个褶皱。还存在许多横向和倾斜断层。研究区目前的地质调查结果是绘制了戈尔斯山脉 Magura Nappe 矿床的地质图。总的来说，高分辨率数字高程模型对该地质研究的进展做出了重大贡献。