Subsolidus Flow
Subsolidus Flow is a geodynamic process denoting the quasi-static, thermally driven deformation and mass transport of solid silicate minerals within the Earth's mantle under high pressure and temperature conditions, occurring in the absence of partial melting, thereby distinguishing it from melt-mediated or viscous flow mechanisms.
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2.8K
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92
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2017–2026
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Leibniz University Hannover
Hanover, Germany
3 h-index
4 publications
76 citations
United States Geological Survey
Reston, United States
3 h-index
4 publications
143 citations

University of Trieste
Trieste, Italy
2 h-index
4 publications
46 citations
Indian Institute of Technology Kharagpur
Kharagpur, India
2 h-index
3 publications
64 citations
University of North Carolina at Chapel Hill
Chapel Hill, United States
2 h-index
3 publications
120 citations

Ames Research Center
Mountain View, United States
2 h-index
2 publications
53 citations
The University of Texas at Austin
Austin, United States
2 h-index
3 publications
42 citations
University of California, Los Angeles
Los Angeles, United States
2 h-index
3 publications
79 citations
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4 publications · 78 citations
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4 publications · 123 citations
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3 publications · 104 citations
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3 publications · 67 citations
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JGR · 3 publications · 383 citations
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