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Traducción y análisis de palabras por inteligencia artificial

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etimología

Qué (quién) es two-sheeted surface - definición

SERIES OF PARALLEL DYKES CHARACTERISTIC OF OCEANIC CRUST

Sheeted dike comples; Sheeted dike complex; Sheeted dyke complexes; Sheeted dike complexes; Sheeted dyke; Sheeted dike

Surface finish

SMALL, LOCAL DEVIATIONS OF A SURFACE FROM A PERFECTLY FLAT IDEAL; DEFINED BY THE THREE CHARACTERISTICS OF LAY, SURFACE ROUGHNESS, AND WAVINESS

Surface texture symbol; Surface texture; Surface topography

Surface finish, also known as surface texture or surface topography, is the nature of a surface as defined by the three characteristics of lay, surface roughness, and waviness.. It comprises the small, local deviations of a surface from the perfectly flat ideal (a true plane).

https://en.wikipedia.org/wiki/Surface_finish

Parametric surface

SURFACE IN THE EUCLIDEAN SPACE

Parametrized surface; Parametrised surface; Parametrized Surface; Surface parameterisation; Parametric object

A parametric surface is a surface in the Euclidean space \R^3 which is defined by a parametric equation with two parameters Parametric representation is a very general way to specify a surface, as well as implicit representation. Surfaces that occur in two of the main theorems of vector calculus, Stokes' theorem and the divergence theorem, are frequently given in a parametric form.

https://en.wikipedia.org/wiki/Parametric_surface

Sheeted dyke complex

A sheeted dyke complex, or sheeted dike complex, is a series of sub-parallel intrusions of igneous rock, forming a layer within the oceanic crust. At mid-ocean ridges, dykes are formed when magma beneath areas of tectonic plate divergence travels through a fracture in the earlier formed oceanic crust, feeding the lavas above and cooling below the seafloor forming upright columns of igneous rock.

https://en.wikipedia.org/wiki/Sheeted_dyke_complex

Wikipedia

Sheeted dyke complex

A sheeted dyke complex, or sheeted dike complex, is a series of sub-parallel intrusions of igneous rock, forming a layer within the oceanic crust. At mid-ocean ridges, dykes are formed when magma beneath areas of tectonic plate divergence travels through a fracture in the earlier formed oceanic crust, feeding the lavas above and cooling below the seafloor forming upright columns of igneous rock. Magma continues to cool, as the existing seafloor moves away from the area of divergence, and additional magma is intruded and cools. In some tectonic settings slices of the oceanic crust are obducted (emplaced) upon continental crust, forming an ophiolite.

https://en.wikipedia.org/wiki/Sheeted dyke complex