By the end of this week, seismologists expect to have a clear understanding of the size and geometry of the fault that ruptured on Sunday. This will then indicate the level of stress change that has occurred on neighbouring faults - those within a 15km radius of yesterday's epicentre.
The faults in Cook Strait have been well mapped by Niwa.
In 2008 Niwa prepared a 36-page report on Cook Strait faults as part of the multi-agency It's Our Fault project. It shows a busy network of faults on the seabed.
There was a small possibility that some of the faults in this region could pose a tsunami threat, so scientists today issued a reminder that if people near the coast felt strong earthquake shaking for 30 seconds or longer, they should move to higher ground.
Seismic engineers are poring over data recorded from networks of instruments installed in Wellington buildings.
The instruments were installed over the past few years, and yesterday's magnitude-6.5 quake was their first major test.
Each of the six structures has instruments placed at different levels to record how various parts of buildings perform during earthquakes. The project jointly involves GNS Science, EQC, the Department of Building and Housing, structural engineering agencies, and university engineering schools. Knowledge gained from the recorded data will help to ensure that design standards of modern buildings can cope with the stresses imposed by strong earthquake-shaking. The buildings are the BNZ building, Wellington Hospital, the Majestic Centre, a high-rise accommodation hall at Victoria University, and the Thorndon flyover.