Dike Propagation
Dike Propagation is a geological process in which molten rock intrudes through fractures in the Earth's crust by fracturing and extending host rock, distinguished from other magma transport mechanisms by its mode of tensile fracture opening and lateral magma migration beneath shield volcanoes.
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8.2K
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299
Authors
167
Institutions
Publications per year
2017–2026
30
116
Magma‐driven propagation of cracks
D. A. Spence, Donald L. Turcotte · Journal of Geophysical Research Atmospheres · 1985 · 372 citations
Dike transport of granitoid magmas
Nick Petford, Ross C. Kerr, John R. Lister · Geology · 1993 · 296 citations
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University of Iceland
Reykjavik, Iceland
11 h-index
22 publications
2.1K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
10 h-index
18 publications
945 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
9 h-index
13 publications
457 citations

Centre National de la Recherche Scientifique
Paris, France
8 h-index
18 publications
867 citations
Roma Tre University
Rome, Italy
8 h-index
14 publications
601 citations
University of Cambridge
Cambridge, United Kingdom
7 h-index
24 publications
1.9K citations
United States Geological Survey
Reston, United States
6 h-index
8 publications
378 citations

Royal Holloway University of London
Egham, United Kingdom
5 h-index
5 publications
342 citations
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JGR · 30 publications · 3.4K citations
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13 publications · 629 citations
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