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

Authors

117

  1. HZ
    Hehua Zhu

    Tongji University, China

    4 publications · 206 citations

    4

    h-index

  2. JG
    Jiateng Guo

    Northeastern University, China

    2 publications · 73 citations

    2

    h-index

  3. HH
    Herbert H. Einstein

    Massachusetts Institute of Technology, United States

    2 publications · 311 citations

    2

    h-index

  4. WF
    Wenkai Feng

    Chengdu University of Technology, China

    2 publications · 60 citations

    2

    h-index

  5. KZ
    Keshen Zhang

    Tongji University, China

    2 publications · 80 citations

    2

    h-index

1–5 of 117

Venues

  1. 10

    h-index

  2. Engineering Geology

    5 publications · 313 citations

    5

    h-index

  3. 4

    h-index

  4. Rock Mechanics and Rock Engineering

    4 publications · 339 citations

    4

    h-index

  5. Computers & Geosciences

    CAGEO · 4 publications · 452 citations

    4

    h-index

1–5