Fault Zone Fluid Pathways
Fault Zone Fluid Pathways is a structural geologic construct denoting a subsurface network of interconnected fractures and permeable zones within a fault system that serves as a conduit for the migration of hydrothermal fluids in oceanic crust.
233
Publications
18.1K
Citations
949
Authors
362
Institutions
Publications per year
2017–2026
54
Parents
233
Fluid flow along potentially active faults in crystalline rock
Mark D. Zoback, Daniel Moos · Geology · 1995 · 966 citations
1–5 of 233
949
4
h-index
4
h-index
4
h-index
4
h-index
3
h-index
1–5 of 949
362

Centre National de la Recherche Scientifique
Paris, France
15 h-index
45 publications
2.5K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
8 h-index
24 publications
1.4K citations

Commonwealth Scientific and Industrial Research Organisation
Canberra, Australia
7 h-index
22 publications
906 citations
University of Utah
Salt Lake City, United States
6 h-index
9 publications
1.8K citations
Total (France)
Paris, France
6 h-index
9 publications
455 citations
Institute of Geosciences and Earth Resources
Pisa, Italy
6 h-index
12 publications
385 citations
United States Geological Survey
Reston, United States
6 h-index
15 publications
2.7K citations
University of Bergen
Bergen, Norway
6 h-index
19 publications
1.7K citations
1–8 of 362
15 publications · 826 citations
14
h-index
15 publications · 790 citations
14
h-index
13 publications · 1.5K citations
13
h-index
12 publications · 2.2K citations
12
h-index
13 publications · 521 citations
12
h-index
1–5