Cite
The Siah Cheshmeh-Khoy-Misho-Tabriz fault (NW Iran) is a cryptic neotethys suture: evidence from detrital zircon geochronology, Hf isotopes, and provenance analysis.
MLA
Mohammadi, Ali, et al. “The Siah Cheshmeh-Khoy-Misho-Tabriz Fault (NW Iran) Is a Cryptic Neotethys Suture: Evidence from Detrital Zircon Geochronology, Hf Isotopes, and Provenance Analysis.” International Geology Review, vol. 64, no. 2, Jan. 2022, pp. 182–202. EBSCOhost, https://doi.org/10.1080/00206814.2020.1845992.
APA
Mohammadi, A., Burg, J.-P., & Guillong, M. (2022). The Siah Cheshmeh-Khoy-Misho-Tabriz fault (NW Iran) is a cryptic neotethys suture: evidence from detrital zircon geochronology, Hf isotopes, and provenance analysis. International Geology Review, 64(2), 182–202. https://doi.org/10.1080/00206814.2020.1845992
Chicago
Mohammadi, Ali, Jean-Pierre Burg, and Marcel Guillong. 2022. “The Siah Cheshmeh-Khoy-Misho-Tabriz Fault (NW Iran) Is a Cryptic Neotethys Suture: Evidence from Detrital Zircon Geochronology, Hf Isotopes, and Provenance Analysis.” International Geology Review 64 (2): 182–202. doi:10.1080/00206814.2020.1845992.