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Core–mantle boundary

Index Core–mantle boundary

The core–mantle boundary (CMB in the parlance of solid earth geophysicists) of the Earth lies between the planet's silicate mantle and its liquid iron-nickel outer core. [1]

20 relations: Beno Gutenberg, Crust (geology), Earthscope, Geophysics, Hotspot (geology), Iron, Keith Edward Bullen, Large low-shear-velocity provinces, Mantle (geology), Nickel, Outer core, P-wave, Planetary core, Post-perovskite, S-wave, Seismic tomography, Seismic wave, Silicate, Silicate perovskite, Ultra low velocity zone.

Beno Gutenberg

Beno Gutenberg (June 4, 1889 – January 25, 1960) was a German-American seismologist who made several important contributions to the science.

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Crust (geology)

In geology, the crust is the outermost solid shell of a rocky planet, dwarf planet, or natural satellite.

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Earthscope

Earthscope is an earth science program using geological and geophysical techniques to explore the structure and evolution of the North American continent and to understand the processes controlling earthquakes and volcanoes.

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Geophysics

Geophysics is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis.

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Hotspot (geology)

In geology, the places known as hotspots or hot spots are volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the surrounding mantle.

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Iron

Iron is a chemical element with symbol Fe (from ferrum) and atomic number 26.

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Keith Edward Bullen

Keith Edward Bullen FAA FRS (29 June 1906 – 23 September 1976) was a New Zealand-born mathematician and geophysicist.

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Large low-shear-velocity provinces

Large low-shear-velocity provinces, LLSVPs, also called LLVPs or superplumes, are characteristic structures of parts of the lowermost mantle (the region surrounding the outer core) of the Earth.

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Mantle (geology)

The mantle is a layer inside a terrestrial planet and some other rocky planetary bodies.

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Nickel

Nickel is a chemical element with symbol Ni and atomic number 28.

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Outer core

The outer core of the Earth is a fluid layer about thick and composed of mostly iron and nickel that lies above Earth's solid inner core and below its mantle.

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P-wave

A P-wave is one of the two main types of elastic body waves, called seismic waves in seismology.

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Planetary core

The planetary core consists of the innermost layer(s) of a planet; which may be composed of solid and liquid layers.

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Post-perovskite

Post-perovskite (pPv) is a high-pressure phase of magnesium silicate (MgSiO3).

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S-wave

In seismology, S-waves, secondary waves, or shear waves (sometimes called an elastic S-wave) are a type of elastic wave, and are one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves.

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Seismic tomography

Seismic tomography is a technique for imaging the subsurface of the Earth with seismic waves produced by earthquakes or explosions.

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Seismic wave

Seismic waves are waves of energy that travel through the Earth's layers, and are a result of earthquakes, volcanic eruptions, magma movement, large landslides and large man-made explosions that give out low-frequency acoustic energy.

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Silicate

In chemistry, a silicate is any member of a family of anions consisting of silicon and oxygen, usually with the general formula, where 0 ≤ x Silicate anions are often large polymeric molecules with an extense variety of structures, including chains and rings (as in polymeric metasilicate), double chains (as in, and sheets (as in. In geology and astronomy, the term silicate is used to mean silicate minerals, ionic solids with silicate anions; as well as rock types that consist predominantly of such minerals. In that context, the term also includes the non-ionic compound silicon dioxide (silica, quartz), which would correspond to x.

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Silicate perovskite

Silicate perovskite (or bridgmanite) is (Mg,Fe)SiO3 and CaSiO3 (calcium silicate) when arranged in a perovskite structure.

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Ultra low velocity zone

Ultra low velocity zones (ULVZs) are patches on the core-mantle boundary that have extremely low seismic velocities.

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Redirects here:

Core mantle boundary, Core-mantle boundary, D Prime Prime Layer, D double-prime, D prime prime, D", D" Zone, D''-layer, D′′ -layer, D′′-layer, D″, D″ Layer, Gutenberg Discontinuity, Gutenberg discontinuity, Wiechert discontinuity, Wiechert-Gutenberg discontinuity.

References

[1] https://en.wikipedia.org/wiki/Core–mantle_boundary

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