Mélange is a mashed-up mixture of rocks, mixed and crushed in a subduction zone. Zones of mélange lie between large areas (miles across) of more coherent rocks of similar type (called terranes) that form larger-scale mixture of rocks that is the Franciscan Complex. Smaller blocks of oceanic crust and sediments and continental marine rocks are mixed together in the mélange and encased in extremely sheared rock that is typically altered to clay.
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Last updated: February 28, 2015