Back-arc basin and Slab pull

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Back-arc basin and Slab pull

Back-arc basin vs. Slab pull

Back-arc basins are geologic basins, submarine features associated with island arcs and subduction zones. Slab pull is the portion of motion of a tectonic plate that can be accounted for by its subduction.

Similarities between Back-arc basin and Slab pull

Back-arc basin and Slab pull have 5 things in common (in Unionpedia): Extensional tectonics, Mantle (geology), Oceanic trench, Plate tectonics, Subduction.

Extensional tectonics

Extensional tectonics is concerned with the structures formed, and the tectonic processes associated with, the stretching of a planetary body's crust or lithosphere.

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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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Oceanic trench

Oceanic trenches are topographic depressions of the sea floor, relatively narrow in width, but very long.

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Plate tectonics

Plate tectonics (from the Late Latin tectonicus, from the τεκτονικός "pertaining to building") is a scientific theory describing the large-scale motion of seven large plates and the movements of a larger number of smaller plates of the Earth's lithosphere, since tectonic processes began on Earth between 3 and 3.5 billion years ago.

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Subduction

Subduction is a geological process that takes place at convergent boundaries of tectonic plates where one plate moves under another and is forced or sinks due to gravity into the mantle.

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The list above answers the following questions

What Back-arc basin and Slab pull have in common
What are the similarities between Back-arc basin and Slab pull

Back-arc basin and Slab pull Comparison

Back-arc basin has 32 relations, while Slab pull has 33. As they have in common 5, the Jaccard index is 7.69% = 5 / (32 + 33).

References

This article shows the relationship between Back-arc basin and Slab pull. To access each article from which the information was extracted, please visit:

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