Evidence for multi-cycle sedimentation and provenance constraints from detrital zircon U–Pb ages: Triassic strata of the Lusitanian basin (western Iberia).

MLA

Pereira, M. F., et al. “Evidence for Multi-Cycle Sedimentation and Provenance Constraints from Detrital Zircon U–Pb Ages: Triassic Strata of the Lusitanian Basin (Western Iberia).” Tectonophysics, vol. 681, June 2016, pp. 318–31. EBSCOhost, https://doi.org/10.1016/j.tecto.2015.10.011.

APA

Pereira, M. F., Gama, C., Chichorro, M., Silva, J. B., Gutiérrez-Alonso, G., Hofmann, M., Linnemann, U., & Gärtner, A. (2016). Evidence for multi-cycle sedimentation and provenance constraints from detrital zircon U–Pb ages: Triassic strata of the Lusitanian basin (western Iberia). Tectonophysics, 681, 318–331. https://doi.org/10.1016/j.tecto.2015.10.011

Chicago

Pereira, M.F., C. Gama, M. Chichorro, J.B. Silva, G. Gutiérrez-Alonso, M. Hofmann, U. Linnemann, and A. Gärtner. 2016. “Evidence for Multi-Cycle Sedimentation and Provenance Constraints from Detrital Zircon U–Pb Ages: Triassic Strata of the Lusitanian Basin (Western Iberia).” Tectonophysics 681 (June): 318–31. doi:10.1016/j.tecto.2015.10.011.