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Τι (ποιος) είναι MAGMATIC - ορισμός
Magmatic lull
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
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.](https://commons.wikimedia.org/wiki/Special:FilePath/Saint-Martin-de-Fressengeas Harzburgit2.jpg?width=200 "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.
Παραδείγματα από το σώμα κειμένου για MAGMATIC
1. The presence of sulfur, one of the main magmatic gases, is a sign that molten rock has moved closer to surface, McNutt said.
2. But I‘m not a drilling expert." The mudflow is thought to have been caused by one of four possibilities: gas–charged fluids breaching coral mounds on top of the limestone rock; a magmatic reaction generating gas; a new–born mud volcano; or hydrothermal fluids migrating from neighbouring areas.