magmatic$46214$ - significado y definición. Qué es magmatic$46214$
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Qué (quién) es magmatic$46214$ - definición

EMPLACEMENT OF MAGMA WITHIN AND AT THE SURFACE OF THE OUTER LAYERS OF A TERRESTRIAL PLANET, WHICH SOLIDIFIES AS IGNEOUS ROCKS
Magmatic activity

Magmatic lull         
Volcanic gap; Magmatic lulls; Volcanic gaps; Magmatic gap; Magmatic gaps
A magmatic lull is a period of declined magmatic activity in volcanically active regions. They may occur as a result of underthrusting of hinterland lithosphere beneath a volcanic arc, changes in subduction parameters such as relative velocity, direction and slab dip (e.
Magmatic underplating         
  • As magma rises up to the surface, some may get trapped at the crust-mantle boundary, accumulating and eventually solidifying, thickening the crust.
TRAPPING OF BASALTIC MAGMAS DURING THEIR RISE TO THE SURFACE AT THE MOHOROVIČIĆ DISCONTINUITY OR WITHIN THE CRUST
Underplating; User:Sjense2/magmatic underplating; Magmatic Underplating
Magmatic underplating occurs when basaltic magmas are trapped during their rise to the surface at the Mohorovičić discontinuity or within the crust. Entrapment (or 'stalling out') of magmas within the crust occurs due to the difference in relative densities between the rising magma and the surrounding rock.
Magmatic foliation         
  • Metaharzburgite from the [[Rebière Massif]], [[Saint-Martin-de-Fressengeas]], [[Dordogne, France]]. The nearly upright magmatic (slightly South dipping) flow foliation parallels the hammer shaft.
FOLIATION IN GRANITOIDS
Magmatic foliations
Magmatic foliation is a term in geology, for foliation in granitoids that form by magmatic flow, "submagmatic flow," by high-temperature solid-state deformation and moderate- to low-temperature solid-state deformation.ScienceDirect: Foliations in granitoids can form by magmatic flow, ‘submagmatic flow’, high-temperature solid-state deformation and moderate- to low-temperature solid-state deformation.

Wikipedia

Magmatism

Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity, the production, intrusion and extrusion of magma or lava. Volcanism is the surface expression of magmatism.

Magmatism is one of the main processes responsible for mountain formation. The nature of magmatism depends on the tectonic setting. For example, andesitic magmatism is associated with the formation of island arcs at convergent plate boundaries while basaltic magmatism is found at mid-ocean ridges during sea-floor spreading at divergent plate boundaries.

On Earth, magma forms by partial melting of silicate rocks either in the mantle, continental or oceanic crust. Evidence for magmatic activity is usually found in the form of igneous rocks formed from magma.