Subsidence history and seismic stratigraphy of the Western Musandam peninsula, Oman-United Arab Emirates Mountains by Ali, M, Aidarbayev, S, Searle, M, Watts, A

“…Seismic reflection profiles, exploratory well, and outcrop data are used to determine the stratigraphy and tectonic subsidence and uplift history of the western Musandam peninsula. Five major regional megasequences have been recognized: (1) Permian to Late Cretaceous rifted margin sequence, (2) Late Cretaceous Aruma foreland basin sequence that evolved in response to the obduction of the Semail Ophiolite, (3) early–mid-Cenozoic Pabdeh foreland basin sequence that formed due to orogenic loading associated with the early continent–continent collision of the Arabian and Eurasian plates in the Zagros mountains of central Iran, (4) a sequence above the mid-Miocene unconformity that marks the final stage of continent–continent collision, and (5) a sequence above the late Pliocene unconformity interpreted as tilting due to the latest stage of continent–continent collision. …”

Subsidence history, gravity anomalies, and flexure of the northeast Australian margin in Papua New Guinea by Haddad, D, Watts, A

A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica by Close, D, Watts, A, Stagg, H

“…Off the central and western Wilkes Land margin, the COTZ extends ∼200 km from the shelf break and encompasses the magnetic anomaly previously interpreted as Chron 34y. …”