Discontinuity Trace Analysis
Discontinuity Trace Analysis is a geological mapping method that identifies, measures, and characterizes the two-dimensional surface expressions of fractures or joints in rock masses to assess their spatial distribution, orientation, and dimensional properties for stability and deformation analysis.
39
Publications
3.1K
Citations
117
Authors
50
Institutions
Publications per year
2017–2026
19
39
Discontinuity analysis for rock engineering
Choice Reviews Online · 1993 · 168 citations
Discontinuity analysis for rock engineering
I. W. Farmer · Journal of Applied Geophysics · 1993 · 144 citations
1–5 of 39
117
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Massachusetts Institute of Technology, United States
2 publications · 311 citations
2
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2
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2
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1–5 of 117
50
Tongji University
Shanghai, China
5 h-index
14 publications
754 citations
China University of Geosciences
Wuhan, China
4 h-index
8 publications
344 citations

Northeastern University
Shenyang, China
3 h-index
13 publications
462 citations
University of Arizona
Tucson, United States
3 h-index
4 publications
380 citations

Imperial College London
London, United Kingdom
3 h-index
3 publications
789 citations

Université Laval
Québec, Canada
2 h-index
6 publications
404 citations

Sichuan University
Chengdu, China
2 h-index
5 publications
182 citations
University of British Columbia, Okanagan Campus
Kelowna, Canada
2 h-index
4 publications
258 citations
1–8 of 50
10 publications · 602 citations
10
h-index
5 publications · 313 citations
5
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4 publications · 813 citations
4
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4 publications · 339 citations
4
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CAGEO · 4 publications · 452 citations
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