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Comparing tiltmeters for crustal deformation measurement--a preliminary report
Summary
Comparing high-precision tiltmeters at Pinon Flat Observatory revealed instrument performance differences. The most stable tilt record showed a potential tectonic deformation rate, but sensor improvements are needed for continuous motion measurement.
Area of Science:
- Geophysics
- Tectonics
- Instrument Science
Background:
- High-precision tiltmeters are crucial for measuring tectonic deformation.
- Instrument comparison is essential for validating measurement techniques.
Purpose of the Study:
- Compare the performance of four different tiltmeters over 1.2 years.
- Assess instrument suitability for measuring tectonic deformation.
- Identify effective measurement techniques and potential improvements.
Main Methods:
- Operated two Michelson-Gale fluid tiltmeters, one center-pressure tiltmeter, and one borehole tiltmeter.
- Collected 1.2 years of high-precision tilt data at Pinon Flat Observatory.
- Analyzed data for coherence and correlation with environmental factors (e.g., air temperature) at nontidal frequencies.
Main Results:
- Michelson-Gale instruments showed limited coherence at 2-4 day periods.
- Center-pressure tiltmeter correlated with air temperature over several days to weeks.
- The most stable instrument recorded a secular tilt rate of 0.28 μrad/a, potentially indicating real tectonic motion.
Conclusions:
- Instrument comparison identified varying levels of success in measurement techniques.
- Low-noise data likely requires complex and expensive instruments.
- Existing tilt sensors require further improvement for continuous tectonic motion measurement.