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
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48
Technology Holding (United States)
Salt Lake City, United States
3 h-index
5 publications
198 citations
Georgia Institute of Technology
Atlanta, United States
2 h-index
5 publications
117 citations
Schlumberger (United States)
Houston, United States
2 h-index
2 publications
37 citations

Monash University
Melbourne, Australia
2 h-index
2 publications
38 citations
Institute of Rock and Soil Mechanics
Wuhan, China
2 h-index
7 publications
601 citations
Tianjin University
Tianjin, China
2 h-index
6 publications
540 citations

Pennsylvania State University
State College, United States
2 h-index
4 publications
86 citations

Centre National de la Recherche Scientifique
Paris, France
1 h-index
3 publications
141 citations
1–8 of 48
3 publications · 102 citations
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3 publications · 163 citations
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2 publications · 130 citations
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2 publications · 53 citations
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2 publications · 84 citations
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1–5