Fault Breccia

Fault breccia is a type of fault rock characterized by angular clasts and fragmented particles formed through brittle deformation within a fault zone, distinguished from other fault rocks by its lack of significant mineral alignment and its genesis via mechanical shattering during seismic slip.

279

Publications

13.1K

Citations

798

Authors

320

Institutions

Publications per year

2017–2026

46

Authors

798

  1. MA
    Michael Alber

    Ruhr University Bochum, Germany

    10 publications · 478 citations

    10

    h-index

  2. SK
    S. Kahraman

    Niğde Ömer Halisdemir Üniversitesi, Türkiye

    10 publications · 478 citations

    10

    h-index

  3. NW
    Nigel Woodcock

    University of Cambridge, United Kingdom

    9 publications · 701 citations

    9

    h-index

  4. JA
    J. A. D. Dickson

    University of Cambridge, United Kingdom

    5 publications · 236 citations

    5

    h-index

  5. MF
    Mustafa Fener

    Niğde Ömer Halisdemir Üniversitesi, Türkiye

    4 publications · 184 citations

    4

    h-index

1–5 of 798

Venues

  1. Journal of Structural Geology

    17 publications · 633 citations

    13

    h-index

  2. Economic Geology

    17 publications · 644 citations

    12

    h-index

  3. Journal of the Geological Society

    JGS · 13 publications · 2.9K citations

    12

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 11 publications · 452 citations

    12

    h-index

  5. Canadian Journal of Earth Sciences

    10 publications · 274 citations

    10

    h-index

1–5