Abstract
Heat, mass, and fluid transfer processes related to the formation and growth of the continental crust along convergent and divergent plate boundaries, and the formation, modification, and recycling of the continental crust are key research themes in the solid Earth Science community. Establishing the link between magma generation, transport, emplacement, and eruption can therefore significantly improve our understanding of crust-forming processes associated with plate tectonics, and, particularly, help determining the architecture, and composition of the Earth's lithosphere.
Highlights
Specialty section: This article was submitted to Volcanology, a section of the journal Frontiers in Earth Science
Establishing the link between magma generation, transport, emplacement, and eruption can significantly improve our understanding of crust-forming processes associated with plate tectonics, and, help determining the architecture, and composition of the Earth’s lithosphere
Establishing the link between magma generation, transport, emplacement, and eruption is essential to significantly improve our understanding of crust-forming processes associated with plate tectonics, and help determine the Earth’s lithosphere architecture, composition, and dynamics
Summary
Specialty section: This article was submitted to Volcanology, a section of the journal Frontiers in Earth Science. Establishing the link between magma generation, transport, emplacement, and eruption can significantly improve our understanding of crust-forming processes associated with plate tectonics, and, help determining the architecture, and composition of the Earth’s lithosphere.
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