Quaternary Thrusting in the Central Oman Mountains-Novel Observations and Causes: Insights from Optical Stimulate Luminescence Dating and Kinematic Fault Analyses

For the first time, Quaternary thrusts are documented within the Central Oman Mountains
to the northwest of the Jabal Akhdar Dome. Thrusts with a throw of up to 1.1 m displace Quaternary
alluvial fan conglomerates. These conglomerates have an Optical Stimulate Luminescence (OSL)
age of 159 ± 7.9 ka BP and were deposited during MIS 6 (Marine Isotope Stage). The thrusts occur
in two sets. Sets 1 and 2 formed during NE/SW and NW/SE shortening, respectively. Set-1-thusts
correlate with the present-day stress field of NE/SW shortening which is related to subduction in
the Makran Subduction Zone, and they strike parallel to the main continuous fold axis of the Jabal
Akhdar and Hawasina windows. Set-2-thrusts correspond to NW/SE shortening and Plio-Pleistocene
contractional structures in the southwestern Jabal Akhdar Dome. Set-2-thrusts are probably related
to local variations of the present-day stress field originating from the Musandam area which is a
part of the Zagros Collision Zone. Both thrust sets mimic the main thrust directions (NW/SE and
NE/SW) within the Permo-Mesozoic allochthonous units (Semail Ophiolite, Hawasina napps) of the
larger study area. The investigated thrusts imply some reactivation of the Hawasina and Semail
thrusts due to far-field stress either from the Makran Subduction Zone and/or the Zagros Collision
Zone. The ongoing tectonic activity of this part of the Oman Mountains, which has been considered
of moderate activity, is for first time identified by structural data as contractional.