Borehole Tilt Results from Charlevoix, Quebec
Abstract
Results from the analysis of recordings from the Charlevoix borehole tilt experiment are presented and discussed. Time variations in the tilt tidal admittance are shown to be related to the time variations in the marine loading from the nearby St. Lawrence estuary. Most of the variability in the sub-tidal tilts is associated with groundwater fluctuations at the Charlevoix site, the residual drift rates varying between 0.01 and 1.0 microrad/yr depending on the tiltmeter. The detectability of coherent regional signals is 2 microrad/yr in the south direction and 0.25 microrad/yr in the east.
Document Details
- Document Type
- Technical Report
- Publication Date
- Apr 23, 1987
- Accession Number
- ADA205824
Entities
People
- Christopher Beaumont
- J. K. L. Peters
- Jochen Kumpel
Organizations
- Dalhousie University