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Strains developed in the hangingwalls of thrusts due to their slip/propagation rate: a dislocation model: discussion |
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| Authors: | CR Tippett PB Jones FR Frey |
| Institution: | Shell Canada Resources Ltd., P.O. Box 100, Station M, Calgary, Alberta, T2P 2H5, Canada;International Tectonic Consultants (ITC) Ltd., 715-4th Street N.W., Calgary, Alberta, T2N 1P3, Canada;Shell Canada Resources Ltd., P.O. Box 100, Station M. Calgary, Alberta, T2P 2H5 Canada |
| Abstract: | Modern seismic data indicate that the sole fault of the Turner Valley thrust sheet does not lose displacement in an up-dip direction and that it does not crop out but rather flattens into the triangle zone on the eastern edge of the Rocky Mountain Foothills Belt. Well constrained balanced cross-sections drawn through this part of the belt do not incorporate significant folding related to the propagation of thrust faults. |
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