Abstract
Inhomogeneous deformation in the vicinity of a lateral contrast between different poroelastic structures in the crust causes local tidal tilt disturbances. A number of model approaches have been published since more than 20 years in order to give a quantitative estimation of this effect which is known as ‘geologic effect’. Most of them correctly predict the general behaviour of tidal tilt modification near an elastic contrast but underestimate the large disturbances that have been observed experimentally. In principle, the geologic effect can be used to infer changes in the state of deformation with increasing tectonic stress. Several experiments have been conducted in earthquake prone areas in order to detect temporal variations of tidal tilt parameters related to seismotectonic events; the results, however, so far are inconclusive.
Tidal tilt observations along a western strand of the North-Anatolian Fault Zone, integrated within an interdisciplinary earthquake research project, reveal considerable deviations of the tidal tilt parameters from the response of a laterally homogeneous Earth. The most prominent temporal phenomenon during the years 1988 to 1994 are seasonal variations of the order of 8% with respect to the tidal tilt residual amplitudes. They are superimposed on a secular drift of the order of 5%, which starts or intensifies in the beginning of 1991. Both classes of signals are correlated with similar changes in independent observables like microseismic activity, the traveltimes of longitudinal waves, the accumulation of tectonic strain and the temperature of ground water. They are interpreted as being caused by changes of effective stress due to fluctuations of internal pore fluid pressure and/or the ambient stress level.
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References
Aggarval, Y. P., L. R. Sykes, Y. Armbruster, and M. L. Sbar. 1973. Premonitory changes in seismic velocities and prediction of earthquakes, Nature, 241: 101–104.
Beaumont, C. 1978. Linear and nonlinear interactions between the earth tide and a tectonically stressed earth. 313–318. In: Applications of geodesy to geodynamics, I. Mueller, ed., Ohio State University Press.
Beaumont, C. and J. Berger. 1974. Earthquake prediction: modification of the Earth tide tilts and strains, Geophys. J. R. Astron. Soc., 39: 111–121.
Biot, M. A. 1941. General theory of three-dimensional consolidation, J. Applied Physics, 1: 155–164.
Bonatz, M., C. Gerstenecker, C. Kistermann, and J. Zschau. 1983. Tilt measurements across a deep fault zone, Proc. Int. 9th Symp. Earth Tides, New York, 695–704.
Brace, W. F., B. W. Paulding, and C. H. Scholz. 1966. Dilatancy in the fracture of crystalline rocks, J. Geophys. Res., 71: 3939–3953.
Byerlee, J. 1993. Model for episodic flow of high-pressure water in fault zones before earthquakes, Geology, 21: 303–306.
Eshelby, J. D. 1957. The determination of the elastic field of an ellipsoidal inclusion, and related problems, Proc. Roy. Soc., 241: 376–396
Gerstenecker, C., J. Zschau, and M. Bonatz. 1985. Finite element modelling of the Hunsrück tilt anomalies — a model comparison, Proc. Int. Symp. Earth Tides, R. Vieira, ed., Madrid, 797–803.
Harkrider, D. G. 1970. Surface waves in multilayered media, 2, Higher mode spectra and spectral ratios from point sources in plane layered earth models, Bull. Seism. Soc. Amer., 60: 1937.
Harrison, J. C., 1976. Cavity and topographic effects in tilt and strain measurements, Jour. Geophys. Res., 81, 319–328.
King, G. C. P., W. Zürn, R. Evans, and D. Emter. 1976. Site corrections for long period seismometers, tiltmeters and strainmeters, Geoph. J. Roy. Astr. Soc., 44: 405–411.
Kirsch, R. and J. Zschau. 1986. The influence of a dilatant region in the Earth's crust on the Earth tide tilt and strain, J. Geophys., 59: 157–163.
Kümpel, H. J. 1982. Neigungsmessungen zwischen Hydrologie und Ozeanographie, PhD thesis, University of Kiel.
Kümpel, H. J. 1989. Verformungen in der Umgebung von Brunnen, Habil. thesis, University of Kiel.
Latynina, L. A. and S. D. Rizaeva. 1976. On Tidal Strain Variations Before Earthquakes, Tectonophysics, 3: 121–127.
Levine, J., C. Meertens, and R. Busby. 1989. Tilt observations using borehole tiltmeters — 1. Analysis of tidal and secular tilt, J. Geophys. Res., 94: 574–586.
Lühr, B.-G., C. Milkereit, R. Meissner, and N. Büyükköse. 1991. Temporal variations of seismic signals within the active seismic experiment in the Mudurnu Valley, Turkey, Proceedings of the International Conference on Earthquake Prediction: State-of-the-Art, Strasbourg, 336–343.
Mao, W. J., C. Ebblin, and M. Zadro. 1989. Evidence for variations of mechanical properties in the Friuli seismic area, Tectonophysics, 170: 231–242.
Meertens, C. M. 1987. Tilt tides and tectonics at Yellowstone National Park, PhD thesis, University of Colorado.
Meissner, R. 1986. The continental crust — a geophysical approach, International Geophysics Series, 34, Academic Press, London.
Michel, G. W. 1994. ‘Neo'-Kinematics along the North-Anatolian Fault, PhD thesis, Tübinger Geowissenschaftliche Arbeiten (TGA), Reihe A, Band 16, University of Tübingen.
Mikumo, T., M. Kato, H. Doi, J. Wada, T. Tanaka, R. Shichi, and A. Yamamoto. 1977. Possibility of temporal variations in Earth tidal strain amplitudes associated with major earthquakes. 123–136. In: Earthquake Precursors: Proceedings of the U.S.-Japan Seminar on Theoretical and Experimental Investigations of Earthquake Precursors, C. Kisslinger and Z. Shuki (eds.), Central Academic Publishers of Japan, Tokyo.
Milkereit, C. 1988. Dilatanz und Anisotropie als spannungsabhängige Phänomene nichtlinearer Elastizität und ihr Einfluß auf seismische Messungen und Erdgezeitenregistrierungen, diploma thesis, University of Kiel.
Mogi, K. 1985. Earthquake Prediction, Academic Press, Tokyo.
Molodensky, S. M. 1983. Local anomalies in amplitude and phase of tidal tilts and deformations, Izvestiya, Earth Physics, 17: 501–505.
Neresov, I. L., A. N. Semyenov, and J. G. Simbireva. 1971. Space-time distribution of the ratio of travel times of compressional and transverse waves in the Garm region. 334–348. In: Experimental Seismology, Sadovsky (ed.), Nauka, Moscow, (in Russian).
Nishimura, E. 1950. On earth tides, Am. Geophys. Union Trans., 31: 357–376
Nur, A. and J. D. Beyerlee. 1971. An exact effective stress law for elastic deformation of rock with fluids, J. Geophys. Res., 76: 6414–6419.
Nur, A. 1972. Dilatancy, pore fluids, and premonitory variations of ts/tp traveltimes, Bull. Seism. Soc. Am., 62: 1217–1222.
Peters, J. and C. Beaumont. 1985. Borehole tilt measurements from Charlevoix, Québec, J. Geophys. Res., 90: 12791–12806.
Rice, J. R. 1983. Constitutive relations for fault slip and earthquake instabilities, Pure appl. Geophys., 121: 443–475.
Scholz, C. H. 1990. The mechanics of earthquakes and faulting, Cambridge University Press.
Scholz, C. H., L. R. Sykes, and Y. P. Aggarval. 1973. Earthquake prediction: a physical basis, Science, 181: 803–810.
Schüller, K. 1977. Tidal analysis by the hybrid least squares frequency domain convolution method. 103–128. In: Proc. Int. 8th Symp. Earth Tides, M. Bonatz and P. Melchior (eds.), Bonn
Schüller, K. 1985. Computer program HYCON.
Tse S. T. and J. R. Rice. 1986. Crustal earthquake instability in relation to frictional constitutive response, J. Geophys. Res., 91: 9452–9472.
Tullis, T. E. 1988. Rock friction constitutive behavior from laboratory experiments and its implications for an earthquake prediction field monitoring program, Pure appl. Geophys., 126: 555–588.
Westerhaus, M. 1996. Tilt and well level tides along an active fault, PhD-Thesis, Scientific-Technical Reports, 5/1996, GeoForschungsZentrum Potsdam.
Westerhaus, M. and J. Zschau. 1989. Tidal tilt modification at the western end of the North-Anatolian Fault Zone: an indication for slow changes of crustal properties. 82–108. In: Turkish-German Earthquake Research Project, J. Zschau and O. Ergunay (eds.), Kiel
Westerhaus, M., W. Welle, N. Büyükköse, and J. Zschau. 1991. Temporal variations of crustal properties in the Mudurnu Valley, Turkey: an indication for regional effects of local asperities?, Proceedings of the International Conference on Earthquake Prediction: State-of-the-Art, Strasbourg, 272–281.
Wyss, M., M. Westerhaus, H. Berckhemer, and R. Ates. 1995. Precursory seismic quiescence in the Mudurnu Valley, North Anatolian Fault Zone, Turkey, Geophys. J. Int., 123: 117–124
Zschau, J., M. Westerhaus, W. Welle, and N. Büyükköse, N. Büyükköse, 1991. Regional strain accumulation from local tidal tilt-and well level data: a new approach, Proceedings of the International Conference on Earthquake Prediction: State-of-the-Art, Strasbourg, 444–453.
Zürn, W., H. Kiesel, H. Otto, and H. Mälzer. 1977. Phenomenological approach to straintilt coupling at Schiltach Observatory. 451–465. In: Proc. 8th Int. Symp. Earth Tides, M. Bonatz and P. Melchior (eds.), Bonn.
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Westerhaus, M. (1997). Tidal tilt modification along an active fault. In: Wilhelm, H., Zürn, W., Wenzel, HG. (eds) Tidal Phenomena. Lecture Notes in Earth Sciences, vol 66. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0011469
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DOI: https://doi.org/10.1007/BFb0011469
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