Detrital zircon SHRIMP U-Pb age study of the Cordillera Darwin Metamorphic Complex of Tierra del Fuego: sedimentary sources and implications for the evolution of the Pacific margin of Gondwana.

MLA

Hervé, F., et al. “Detrital Zircon SHRIMP U-Pb Age Study of the Cordillera Darwin Metamorphic Complex of Tierra Del Fuego: Sedimentary Sources and Implications for the Evolution of the Pacific Margin of Gondwana.” Journal of the Geological Society, vol. 167, no. 3, May 2010, p. 10. EBSCOhost, https://doi.org/10.1144/0016-76492009-124.

APA

Hervé, F., Fanning, C. M., Pankhurst, R. J., Mpodozis, C., Klepeis, K., Calderón, M., & Thomson, S. N. (2010). Detrital zircon SHRIMP U-Pb age study of the Cordillera Darwin Metamorphic Complex of Tierra del Fuego: sedimentary sources and implications for the evolution of the Pacific margin of Gondwana. Journal of the Geological Society, 167(3), 10. https://doi.org/10.1144/0016-76492009-124

Chicago

Hervé, F., C. M. Fanning, R. J. Pankhurst, C. Mpodozis, K. Klepeis, M. Calderón, and S. N. Thomson. 2010. “Detrital Zircon SHRIMP U-Pb Age Study of the Cordillera Darwin Metamorphic Complex of Tierra Del Fuego: Sedimentary Sources and Implications for the Evolution of the Pacific Margin of Gondwana.” Journal of the Geological Society 167 (3): 10. doi:10.1144/0016-76492009-124.