Technical description of solution ausd04it.snx 1. Purpose: VLBI session files in SINEX 2.0 format, including epoch coordinates and EOP. 2. Analysis Center: GEOSCIENCE AUSTRALIA (AUS) 3. Short narrative description of solution: Observational VLBI data files including all networks since 1983 have been analyzed for this solution. Reductional model is realised in accordance with IERS Conventions (2000) except recommended precession/nutation model. Celestial reference frame was fixed to ICRF Ext.2 catalogue. The Terrestrial Reference Frame is defined by no-net-translation and rotation constraints for the coordinates of all sites in a VLBI session related to VTRF2003. The values of the official list of VLBI antenna axis offsets issued by the IVS Analysis Coordinator. All parameters under estimation have been adjusted using Kalman filter technique. Tropospheric gradients have been considered as constant parameters. 4. Estimated parameters: a. celestial frame: No b. terrestrial frame: Yes c. Earth orientation: X, Y, UT1-UTC, X-dot, Y-dot, LOD, dpsi, deps d. zenith troposphere: Random walk process e. troposphere gradients: Estimates as a constant parameters f. station clocks: Offset as a random walk process, rate as a constant except sessions when the clock rate is considered as a random walk process for separate stations g. baseline clocks: No h. other: No 5. Celestial reference frame: a. a priori source positions: ICRF Ext.2 solution b. source positions adjusted in solution: No e. solution identification or reference: ICRF Ext.2 6 - Terrestrial reference frame: a. a priori station positions: VTRF2003 ITRF solution imposed by NNR, NNT constraints. b. a priori station velocities: VTRF2003 solution c. reference epoch: 1997.0 d. station positions/velocities adjusted in solution: station positions adjusted on daily basis l. solution identification or reference: VTRF2003 7. Earth orientation: a. a priori precession model: IAU(1976) b. a priori nutation model: IAU(1980) c. a priori short-period tidal variations in x, y, UT1: IERS Conventions (2000) - model by R.Eanes d. EOP estimation: X, Y, UT1-UTC, dpsi, deps for each session 8. A priori geophysical models: a. troposphere: Vienna mapping function for dry and wet delays b. solid Earth tide: IERS Conventions 2000, except re-instating for permanent tides. c. ocean loading: IERS Conventions 2000 d. atmosphere loading: No 9. Data type: delays 10. Data editing: Only data with zero quality flag in NGS format are used 11. Data weighting: Observations with elevation less than 5 degrees to be divided by sin(elevation). Observations with elevation more than 5 degrees are not weighted as a rule, but Kalman filter approach checks a quality of every observation and downweights it in case of bad result. 12. Standard errors reported: Formal errors are derived from Kalman filter adjustment 13. Software: OCCAM 6.0 development 14. Other information: Gilcreek after the seismic event 03-Nov-2002 has the following shift for apriori coordinates. radial = 8.0 mm latitude = -47.8 mm longitude = 22.6 mm Moreover, exponential model has been applied for post-seismic effect approximation