Tidal and coseismic well-level observations at the Charlevoix Geophysical Observatory, Quebec

A systematic change in well tide amplitude and phase during the period 1981–1986 suggests a progressive attenuation of tidal strain in the azimuth range 135°–165° east of north. This may be related to an increasing concentration of tidal strain at one or more nearby NE-striking faults or to a change...

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Veröffentlicht in:	Tectonophysics 1989-10, Vol.167 (2), p.349-361
1. Verfasser:	Bower, D.R.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Natural hazards: prediction, damages, etc
Online-Zugang:	Volltext
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