机译:李斯特与平面法向断层几何关系:以艾森斯塔特-索普朗盆地(奥地利)为例
Department for Geodynamics and Sedimentology, University ofVienna, Althanstrasse 14, 1090 Vienna, Austria;
Department for Geodynamics and Sedimentology, University ofVienna, Althanstrasse 14, 1090 Vienna, Austria;
Institute of Geodesy and Geophysics, Vienna University of Technology, Gusshausstrasse 27-29, 1040 Vienna, Austria;
Department for Geodynamics and Sedimentology, University ofVienna, Althanstrasse 14, 1090 Vienna, Austria;
Christian Doppler Laboratory for 'Spatial Data from Laser Scanning and Remote Sensing', Vienna University of Technology, Gusshausstrasse 27-29, 1040 Vienna, Austria;
Department for Geodynamics and Sedimentology, University ofVienna, Althanstrasse 14, 1090 Vienna, Austria;
listric fault; fault drag; ground penetrating radar; balanced cross-section;
机译:EISENSTADT-SOPRON盆地边缘多相正常断裂是空间有限煤微型油气田(东奥地利)的控制因素
机译:亚利桑那州东南部的Eagle Pass支队:南部盆地和山脉中的中新世中层利斯特(?)正断层的产物
机译:新西兰北塔纳崎盆地脚趾地区脚下缩短的构造压实缩短
机译:洞穴故障对COSO地热场骨折形成的影响
机译:列表型正常断层系统中的传输带。
机译:控制与断层相关的正常背斜线形成上的断层平面几何形状:一种实验方法
机译:预先存在的正常故障如何影响裂缝几何形状?挪威罗弗敦边缘底层底层结构与邻近盆地的比较
机译:Listric法向断裂的有限元建模