Figure 7. Structural map of the Muscat-Seeb area of Figure 4. Most of the black folds/faults are of post-mid-Eocene age; (a) – Le Métour et al. (1986a, 1986b); (b) – Rabu et al. (1986); (c) – Villey et al. (1986a); (d) – Villey et al. (1986b); (e) – Coffield (1990); (f) – Miller et al. (2002); (g) – Fournier et al. (2006); (h) – Kajima et al. (2012a); (i) – Kajima et al. (2012b); (j) – Kajima et al. (2012c); (k) 10 – Scharf et al. (2016); (l) – Mattern et al. (2018c); (m) – Mattern et al. (2020a); (n) – Levell et al. (2021). Thin black lines represent undifferentiated faults, taken from Béchennec et al. (1986), Villey et al. (1986a, 1986b), Le Métour et al. (1986b) and Rabu et al. (1986). The age of these faults is unknown. Note that the large NNE-oriented anticline as continuation of the Jabal Akhdar/Jabal Nakhl is late Eocene in age, based on seismic data (Levell et al., 2021).