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The Qinling Orogenic Belt was formed by long-lived subduction and collision between the North and South China blocks. Our 40 Ar/ 39 Ar geochronological data of amphibole, white mica, and biotite reveal different exhumation and cooling histories of the major units in the North Qinling Belt and South Qinling Belt (SQB), constraining the multiple orogenic processes. The exhumation of the Qinling Group in the North Qinling Belt started before 432 Ma, through about 500°C during 432.3-405 Ma, followed by rapid cooling below 425°C at 388.9 ± 1.1 Ma and slow cooling through about 300°C during 333.3-329.5 Ma. A similar exhumation history of the Kuanping Group started from about 383 Ma, cooled below 425°C at 364.9 ± 1.2 Ma and 300°C at 341.8 ± 1.3 Ma. The metamorphic fore-arc sedimentary wedge cooled below 500°C during 322-311.2 Ma, below 425°C at 306.3 ± 2.8 Ma, and 300°C at 249 ± 2.8 Ma. However, the white mica 40 Ar/ 39 Ar ages of 349.4 ± 5.1 and 363.2 ± 2.5 Ma constrain the syntectonic metamorphic crystallization age of the Devonian Liuling Group in the northern SQB, whereas 228.2 ± 0.7 Ma indicates either a delayed cooling of the Wudang Group in the southern SQB or a second stage of low-temperature thermal overprint. Together with previous cooling ages and regional geology, our new data support a tectonic model of Early Paleozoic Andean-type orogeny with subsequent Late Paleozoic continental subduction in the Qinling Orogenic Belt. 40 Ar/ 39 Ar dating. Tectonics, 37, 4037-4067. https://doi.

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