Lg coda Q and its relation to the geology and tectonics of the Middle East

Regional seismograms were collected to image the lateral variations of Lg coda Q at 1 Hz (Q(0)) and its frequency dependence (eta) in the Middle East using a back-projection method. The data include 124 vertical-component traces recorded at 10 stations during the period 1986-1996. The resulting images reveal lateral variations in both Q(0) and eta. In the Turkish and Iranian Plateaus, a highly deformed and tectonically active region, Q(0), ranges between about 150 and 300, with the lowest values occurring in western Anatolia where extremely high heat Bow has been measured. The low Q(0) values found in this region agree with those found in other tectonically active regions of the world. Throughout most of the Arabian Peninsula, a relatively stable region, Q(0) varies between 350 and 450, bring highest in the shield area and lowest in the eastern basins. All values are considerably lower than those found in most other stable regions. Low Q values throughout the Middle East may be caused by interstitial fluids that have migrated to the crust from the upper mantle, where they were probably generated by hydrothermal reactions at elevated temperatures known to occur there. Low Q(0) values (about 250) are also found in the Oman folded zone, a region with thick sedimentary deposits. eta varies inversely with Q(0) throughout most of the Middle East, with lower values (0.4-0.5) in the Arabian Peninsula and higher values (0.6-0.8) in Iran and Turkey. Q(0) and eta are both low in the Oman folded zone and western Anatolia.