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In geology, a terrane refers to the area or surface where a particular rock or group of rocks is prevalent. It is essentially the terrain or landform associated with specific geological materials.12

The concept of terranes is also used in plate tectonics to describe fragments of crust, such as island arcs or microcontinents, that have been displaced from their original location and attached to a larger continental mass. This process, known as accretionary tectonics, occurs at subduction zones where denser oceanic plates are pulled beneath continental plates. These displaced fragments are called allochthonous terranes.3

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