The sequence of rocks that comprise an accretionary wedge is called an ophiolite.

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An ophiolite is a sequence of rocks that is typically found in oceanic crust that has been uplifted and obducted onto continental crust. An accretionary wedge is a type of geologic feature that develops at subduction zones, and is composed of a mixture of sedimentary and volcanic rocks, including sandstone, shale, basalt, and other rock types.

The Sequence of Rocks That Comprise an Accretionary Wedge Is