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Geology; February 2006; v. 34; no. 2; p. 97-100; DOI: 10.1130/G21929.1
© 2006 Geological Society of America
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Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks

Amy L. Weislogel1, Stephan A. Graham1, Edmund Z. Chang1, Joeseph L. Wooden2, George E. Gehrels3 and Hengshu Yang4

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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