کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4692181 1636782 2013 16 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Structural characterization of Turtle Mountain anticline (Alberta, Canada) and impact on rock slope failure
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
Structural characterization of Turtle Mountain anticline (Alberta, Canada) and impact on rock slope failure
چکیده انگلیسی


• Remote methods such as TLS and ALS are powerful tools for detailed structural analyses.
• Five sets of fractures occurred during folding event, three are post-folding.
• Fold geometry variation along axis induces variation of the fractures properties.
• Small-scale instabilities mainly controlled by fold geometry and related fracturing
• Large rock slope failure allowed by tectonic induced rock mass strength reduction

This paper proposes a structural investigation of the Turtle Mountain anticline (Alberta, Canada) to better understand the role of the different tectonic features on the development of both local and large scale rock slope instabilities occurring in Turtle Mountain. The study area is investigated by combining remote methods with detailed field surveys. In particular, the benefit of Terrestrial Laser Scanning for ductile and brittle tectonic structure interpretations is illustrated. The proposed tectonic interpretation allows the characterization of the fracturing pattern, the fold geometry and the role of these tectonic features in rock slope instability development. Ten discontinuity sets are identified in the study area, their local variations permitting the differentiation of the study zone into 20 homogenous structural domains. The anticline is described as an eastern verging fold that displays considerable geometry differences along its axis and developed by both flexural slip and tangential longitudinal strain folding mechanisms. Moreover, the origins of the discontinuity sets are determined according to the tectonic phases affecting the region (pre-folding, folding, post-folding). The localization and interpretation of kinematics of the different instabilities revealed the importance of considering the discrete brittle planes of weakness, which largely control the kinematic release of the local instabilities, and also the rock mass damage induced by large tectonic structures (fold hinge, thrust).

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 605, 11 October 2013, Pages 133–148
نویسندگان
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