The Central Asian Orogenic Belt (CAOB, also known as the Central Asian Foldbelt (CAFB), or the Altaids) is one of the largest accretionary orogens on Earth and evolved over some 800 million years from the latest Mesoproterozoic to the early Triassic. It contains a record of geodynamic processes during one of the most important episodes of continental growth in Phanerozoic time.
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