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1 Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305, USA
2 U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025, USA
3 Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
4 Sichuan Bureau of Geology and Ore Examination, Mianyang, Sichuan 621000, People's Republic of China
Using detrital zircon geochronology, turbidite deposystems fed from distinct sediment sources can be distinguished within the Songpan-Ganzi complex, a collapsed Middle to Late Triassic turbidite basin of central China. A southern Songpan-Ganzi deposystem initially was sourced solely by erosion of the Qinling-Dabie orogen during early Late Triassic time, then by Qinling-Dabie orogen, North China block, and South China block sources during middle to late Late Triassic time. A northern Songpan-Ganzi system was sourced by erosion of the Qinling-Dabie orogen and the North China block throughout its deposition. These separate deposystems were later tectonically amalgamated to form one complex and then uplifted as the eastern Tibet Plateau.
Key Words: turbidite collisional orogen unroofing detrital zircon China
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