Crustal deformation
SAR (ALOS-2 satellite)-derived crustal deformation
- Data format: GeoTIFF
- Unit: cm
| Data | File | Note |
|---|---|---|
| 2-D (quasi-EW, quasi-UD) | qEW.tif qUD.tif | - Eastward and upward: positive sign - Fig. 5 in Kobayashi et al. (2018) |
| InSAR (unwrapped) |
20160809-20171114.insar_unwrap.tif 20171004-20171115.insar_unwrap.tif |
- File name: [YYYYMMDD1-YYYYMMDD2]. insar_unwrap.tif - Fig. 2 & 3 in Kobayashi et al. (2018) - YYYYMMDD1: Acquisition date of 1st image - YYYYMMDD2: Acquisition date of 2nd image |
| Unit vector: for InSAR (range component) |
20160809-20171114.uew_rng.tif 20171004-20171115.uew_rng.tif 20160809-20171114.uns_rng.tif 20171004-20171115.uns_rng.tif |
- File name: [YYYYMMDD1-YYYYMMDD2].uew_rng.tif (EW) - File name: [YYYYMMDD1-YYYYMMDD2].uns_rng.tif (NS) |
Fault model
Slip distribution model
- Data format: ASCII
- The first line is a header that explaines parameters for each column
- File format (from left): Fault number, Longitude [deg], Latitude [deg], Depth [km], Length [km], Width [km], Strike [deg], Dip [deg], Rake [deg], Slip amount [m].
- Longitude, latitude and depth represent the central position of fault patch
- Strike angle is measured clockwise from the north
| Data | File | Note |
|---|---|---|
| Slip distribution model | fault_slip.dat |
Citation
- Kobayashi, T., Y. Morishita, H. Yarai, and S. Fujiwara (2018), InSAR-derived Crustal Deformation and Reverse Fault Motion of the 2017 Iran-Iraq Earthquake in the Northwest of the Zagros Orogenic Belt, Bull.Geospatial Info. Auth., 66, 1-9. doi:10.57499/BULLETIN_066_01