构造窗
构造窗（德语：fenster）是指推覆体或大型逆掩断层的上盘岩席在侵蚀作用下蚀穿断层面，使下盘岩石局部出露地表形成的上盘岩席环绕、四周以断层线为界的下盘局部露头[1]。大小可以从几米到数百公里，典型的构造窗的是东阿尔卑斯山脉的陶恩构造窗（亦称上陶恩山构造窗）[2]和西喀尔巴阡山脉的 Hrzdavá dolina 构造窗[3][4]。
参考文献
- ^ Twiss, Robert J. and Eldridge M. >Moores, Structural Geology, W. H. Freeman, 1992, p. 36 ISBN 978-0716722526
- ^ 《地球科学大辞典》编委会. 地球科学大辞典 基础学科卷. 地质出版社. 2005-11-01: 874. ISBN 9787116046702.
- ^ Schmid, S.M., Scharf, A., Handy, M.R., Rosenberg, C.L., 2013, The Tauern Window (Eastern Alps, Austria): a new tectonic map, with cross-sections and a tectonometamorphic synthesis. Swiss Journal of Geosciences, 106, 1–32, https://doi.org/10.1007/s00015-013-0123-
- ^ Vojtko, R., Králiková, S., Jeřábek, P., Schuster, P., Danišík, M., Fügenschuh, B., Minár, J., Madarás, J., 2016, Geochronological evidence for the Alpine tectono-thermal evolution of the Veporic Unit (Western Carpathians, Slovakia). Tectonophysics, 666, 48-65, https://doi.org/10.1016/j.tecto.2015.10.014