Magma Accumulation
Magma Accumulation is the process by which molten rock generated in the mantle or crust is stored and concentrated in subsurface reservoirs or sill-like structures within volcanic plumbing systems, distinguished from related magmatic processes by its focus on the spatial and temporal coalescence of magma in discrete zones prior to potential eruption or solidification.
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Continental breakup in magmatic provinces: An Ethiopian example
C. J. Ebinger, M. Casey · Geology · 2001 · 498 citations
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Centre National de la Recherche Scientifique
Paris, France
22 h-index
62 publications
4.5K citations
United States Geological Survey
Reston, United States
21 h-index
38 publications
4.5K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
18 h-index
78 publications
4K citations

Institut de physique du globe de Paris
Paris, France
11 h-index
20 publications
1.1K citations

University of Bristol
Bristol, United Kingdom
11 h-index
22 publications
2K citations
University of Geneva
Geneva, Switzerland
11 h-index
20 publications
2.1K citations
Institut de Recherche pour le Développement
Marseille, France
10 h-index
23 publications
928 citations

University of Auckland
Auckland, New Zealand
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12 publications
758 citations
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JGR · 21 publications · 2.1K citations
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