We present the up-to-date seismicity associated with the Turkmanchay-Ardabil section as a series of space-time sections. The aim is to reveal the hidden orders and to facilitate prompt interpretation. The earthquake data is obtained from the IRSC, KOERI-RETMC and USGS databases every minute. With new earthquakes the figures and maps are updated immediately; otherwise, they are regenerated every hour. The following points should be considered regarding the images.
- There are 8 figures showing time-space sections of seismicity for different periods. Earthquakes are projected on the line segments that represent the Turkmanchay-Ardabil section.
- The yellow line segments, ‘SW-NE’, on the maps show the section. Earthquakes within a 20 km range are projected in the section.
- For each figure X, there are 3 associated illustrations with a corresponding period. Xa shows the seismicity for the whole region, while Xb displays the events in the window around the section. Figure Xc shows the depth distribution of events along the section. Their links are given below each figure.
- The thick red line segment, labeled U, on the maps and also along the right axis of each figure represents an uncertain barrier. Provided that a fault line passes along the section, then it turns into a barrier. Therefore, it is essential to determine the mechanism of a couple of events that occurred in the middle of the barrier in 2009 (Figure 6).
- The thick red unlabeled line segment on the maps is a barrier along the North Tabriz fault.
- The earthquake data for the post-2006 period is obtained from the IRSC catalog.
- The earthquake data for 1980 to 2006 is obtained from the KOERI database.
- The earthquake data for the period before 1980 is taken from the USGS database.
- The section is along one of the nodal planes, (strike=212, dip=82, slip=-5), of the 2019/11/07 Turkmanchay earthquake.
Acknowledgment
The earthquake data for this project is obtained from (i) the “Iranian Seismological Center” (IRSC) of the Institute of Geophysics, University of Tehran, (ii) the “Regional Earthquake-Tsunami Monitoring Center” (RETMC) of the Kandilli Observatory and Earthquake Research Institute and (iii) the US Geological Survey (USGS). We appreciate these institutions for the release of their products to the public. The figures are produced by using the “Generic Mapping Tool” (GMT) and we thank the developers of the software (Wessel et al., 2013).
References
- Wessel P, Smith WH, Scharroo R, Luis J, Wobbe F. Generic mapping tools: improved version released. Eos, Transactions American Geophysical Union. 2013;94:409–410.