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By G. P?lmason

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Published by way of the yank Geophysical Union as a part of the Geodynamics Series.

During the prior decade of the overseas Geodynamics application many guides facing particular rift components of the Earth's floor have seemed. such a lot of them symposia that have been held within the respective rift zones. one of the rifts therefore handled are the Rhinegraben, Afar, Iceland, the Baikal rift, the Oslo paleorift, the Rio Grande rift and the lifeless Sea rift. moreover, courses facing reviews of the sea ground have mentioned many oceanic rift components.

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It appears that the geodetic observations to date fail to show significant horizontal component of deformation while the vertical component is convincingly demonstrated. Inside the Rhine graben subsidence dominates. The average northern part of shear deformation. These include gravity and gravity gradient observations, tilt observations, precision leveling, triangulation, and distance measurements (M•lzer left-lateral (Ahorner, 1975). 7 mm/year (Ahorner, 1975). This indicates that most of the geodetic slip rate occurs as a seismic creep, or else, that it occurs in few large earthquakes, none of which Concluding treated Focal some widening major part of movement periods of low activity.

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Geo•hys. Res. 79, A tentative origin of "Transform remarks on the term). Contr. Structural earthquake 81, 41-60, 1970. Turcotte, 2573-2577, Trans. Roy. Soc. London, A268, 423-441, 1971. , Shido, F. and M. a. nd GeophD. , Holland, 167-194, 1978. Sutton, G. , and E. Berg, Seismological studies of the western rift valley of Africa, Trans. Amer. Geophys. Union 39, 474-481, 1958. contraction Muelberger, W. , The Erabuds Fault between Pilar Arroyo Hondo, New Mexico: an active intercontinental transform fault, New Mexico Geol.

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