Tufa Formation

Tufa Formation is a carbonate depositional process characterized by the precipitation of porous, freshwater travertine-like calcium carbonate from ambient temperature waters, typically associated with springs, streams, or lacustrine environments, distinguished from similar carbonate formations by its low-magnesium calcite mineralogy and macroscopic porosity resulting from biologically mediated and abiotic chemical processes.

158

Publications

6.8K

Citations

457

Authors

243

Institutions

Publications per year

2017–2026

20

Authors

457

  1. NH
    Nada Horvatinčić

    Ruđer Bošković Institute, Croatia

    5 publications · 262 citations

    5

    h-index

  2. RC
    Richard C. Preece

    University of Cambridge, United Kingdom

    5 publications · 223 citations

    5

    h-index

  3. BJ
    Brian Jones

    University of Alberta, Canada

    4 publications · 319 citations

    4

    h-index

  4. AG
    Andrew Goudie

    University of Oxford, United Kingdom

    4 publications · 167 citations

    4

    h-index

  5. RN
    Russell N. Drysdale

    The University of Melbourne, Australia

    4 publications · 259 citations

    4

    h-index

1–5 of 457

Venues

  1. Sedimentology

    16 publications · 957 citations

    15

    h-index

  2. Sedimentary Geology

    11 publications · 718 citations

    11

    h-index

  3. 8

    h-index

  4. Journal of Sedimentary Research

    JSR · 7 publications · 475 citations

    7

    h-index

  5. Quaternary Research

    QR · 5 publications · 306 citations

    5

    h-index

1–5