anorlunda said:
Summary:: New ways to use GPS for scientific purposes.
- Feel an earthquake (@davenn will like this)
Thanks for the heads-up
It's more about ...
—to track geologic processes that happen on much slower scales, such as the rate at which Earth’s great crustal plates grind past one another in the process known as plate tectonics. So GPS might tell scientists the speed at which the opposite sides of the San Andreas Fault are creeping past each other, while seismometers measure the ground shaking when that California fault ruptures in a quake.
This has been getting done since the early 1990's. I remember when I doing geology at university back
then, one of the lecturers giving a public talk on how this was being implemented. At the time, for most of
us, this was WOW and COOL. And now, over the last 25 years, this has become just a common thing to do.
GPS quality has been improved and with many more satellites up there now ( not even mentioned in that
article) There are a number of constellations. The two major ones -- GPS - USA, GLONASS - Russia, Now
more recently - BeiDou - China and Galileo - Europe. And a couple of other countries with just a few sat's
up there - IRNSS - India and QZSS - Japan.
Who knew that 20 years later, 2011, I would start working in this field of high precision GPS.
A few basic facts, car/handheld GPS units - ~ 5 - 10m accuracy. Even our high precision units, when
used on their own, are only ~ 1 - 5m accuracy. This precision gear is never used on its own, rather it is
connected to a local GPS base station by either radio or internet, where it can receive GPS corrections
and get much higher accuracy. Originally
Differential GPS was used and it improved accuracies from
several metres down to several cm. This was further improved by incorporating
RTK positioning.
This improved accuracy even more and it is now easy to get down to 2-3mm horizontal positioning.
Vertical positioning is usually always around 2 to 3 times less accurate than horizontal eg. 2-3mm Hz
would give around 5 - 7mm vertical accuracy.
Now, to put this into use, when studying geological plate tectonics. Take a plate boundary like the
San Andreas Fault in California, USA or the Alpine Fault in the South Island of New Zealand.
It is quite easy to measure the 2 significant motions along that boundary even before an earthquake
occurs. And after a quake occurs, then very accurate measurements of the motion can be measured.
Lets look at a drawing as well as an actual fault.
In the above drawing ( a represation of the Alpine Fault in NZ) I have shown relative ground motions
close to and away from the faultline. This fault isn't pure strike-slip, rather there is a component of
compression and so it is called an oblique-slip fault.
At the fault, there is no motion at all and as you move away from the fault axis, the relative ground
motion continues as indicated by the size of the arrows. When the fault finally ruptures, all that motion
that has been occurring away from the fault then releases at the fault and it "catches up".
The ongoing ground motion at position 4 is much more substantial than at position 3 or 2. And for the
Alpine Fault, the motion is ~ 40mm / year. This motion is far above the 2 - 3 mm accuracy noise of the
GPS system so is easily measured and graphed.
The above image shows just a small, ~ 150 - 200km section of the Alpine Fault. It can be seen as that
line in the topography running from lower left to upper rightOK I will leave it at that before I hijack the thread too muchDave