Fracture-controlled Fluid Flow

Fracture-Controlled Fluid Flow is a hydrogeological process in which the movement of fluids within volcanic hydrothermal systems is predominantly governed by the connectivity, geometry, and permeability of fractures, distinguishing it from porous-medium-dominated flow by emphasizing structurally constrained pathways for fluid transport.

38

Publications

1.5K

Citations

107

Authors

48

Institutions

Publications per year

2017–2026

9

Authors

107

  1. SA
    S. A. Holditch

    Mitchell Institute, United States

    3 publications · 95 citations

    3

    h-index

  2. RP
    R. P. Lowell

    Georgia Institute of Technology, United States

    2 publications · 51 citations

    2

    h-index

  3. XH
    Xiaoxue Huang

    Tianjin University, China

    2 publications · 180 citations

    2

    h-index

  4. YH
    Yuanyuan He

    Institute of Rock and Soil Mechanics, China

    2 publications · 180 citations

    2

    h-index

  5. JZ
    Jialing Zhu

    Tianjin University, China

    2 publications · 180 citations

    2

    h-index

1–5 of 107

Venues

  1. Geothermics

    3 publications · 102 citations

    3

    h-index

  2. Applied Thermal Engineering

    3 publications · 163 citations

    3

    h-index

  3. Renewable Energy

    2 publications · 130 citations

    2

    h-index

  4. Geophysical Research Letters

    2 publications · 53 citations

    2

    h-index

  5. Environmental Earth Sciences

    2 publications · 84 citations

    2

    h-index

1–5