The zircon evidence of temporally changing sediment transport-the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara).

MLA

Gärtner, Andreas, et al. “The Zircon Evidence of Temporally Changing Sediment Transport-the NW Gondwana Margin during Cambrian to Devonian Time (Aoucert and Smara Areas, Moroccan Sahara).” International Journal of Earth Sciences, vol. 106, no. 8, Nov. 2017, pp. 2747–69. EBSCOhost, https://doi.org/10.1007/s00531-017-1457-x.

APA

Gärtner, A., Youbi, N., Villeneuve, M., Sagawe, A., Hofmann, M., Mahmoudi, A., Boumehdi, M., & Linnemann, U. (2017). The zircon evidence of temporally changing sediment transport-the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara). International Journal of Earth Sciences, 106(8), 2747–2769. https://doi.org/10.1007/s00531-017-1457-x

Chicago

Gärtner, Andreas, Nasrrddine Youbi, Michel Villeneuve, Anja Sagawe, Mandy Hofmann, Abdelkader Mahmoudi, Moulay Boumehdi, and Ulf Linnemann. 2017. “The Zircon Evidence of Temporally Changing Sediment Transport-the NW Gondwana Margin during Cambrian to Devonian Time (Aoucert and Smara Areas, Moroccan Sahara).” International Journal of Earth Sciences 106 (8): 2747–69. doi:10.1007/s00531-017-1457-x.