Fracture Flow Paths is a subsurface flow pathway mechanism defined as a preferential conduit for fluid movement through discontinuities in geological formations, distinguished from matrix and conduit flow by its reliance on hydraulically conductive fractures or fissures within low-permeability rock masses.
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196
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2017–2026
36
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144
1–5 of 144
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487
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196
Centre National de la Recherche Scientifique
Paris, France
8 h-index
20 publications
1.1K citations
Lawrence Berkeley National Laboratory
Berkeley, United States
7 h-index
20 publications
504 citations
Japan Organization for Metals and Energy Security (Japan)
Tokyo, Japan
4 h-index
9 publications
371 citations
Purdue University West Lafayette
West Lafayette, United States
3 h-index
9 publications
336 citations
ETH Zurich
Zurich, Switzerland
3 h-index
13 publications
373 citations
Monash University
Melbourne, Australia
3 h-index
7 publications
341 citations
University of Liverpool
Liverpool, United Kingdom
3 h-index
3 publications
66 citations
Schlumberger (British Virgin Islands)
Road Town, British Virgin Islands
3 h-index
12 publications
284 citations
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- Water Resources Research
17 publications · 1.4K citations
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- International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts
5 publications · 372 citations
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- Ground Water
GW · 5 publications · 195 citations
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- Engineering Geology
4 publications · 160 citations
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- Geophysical Research Letters
4 publications · 174 citations
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