構造窗
構造窗（德語：fenster）是指推覆體或大型逆掩斷層的上盤岩席在侵蝕作用下蝕穿斷層面，使下盤岩石局部出露地表形成的上盤岩席環繞、四周以斷層線為界的下盤局部露頭[1]。大小可以從幾米到數百公里，典型的構造窗的是東阿爾卑斯山脈的陶恩構造窗（亦稱上陶恩山構造窗）[2]和西喀爾巴阡山脈的 Hrzdavá dolina 構造窗[3][4]。
參考文獻
[編輯]- ^ Twiss, Robert J. and Eldridge M. >Moores, Structural Geology, W. H. Freeman, 1992, p. 36 ISBN 978-0716722526
- ^ 《地球科學大辭典》編委會. 地球科学大辞典 基础学科卷. 地質出版社. 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