C. Cramez, Switzerland

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32Self-similarityOn this line of Gulf of Mexico, self-similarity is paramount in turbidite depositional systems. Indeed, inslope fans, channel-levees complexes (whole) are composed by a multitude of parts with same shape andstructure in spite of their small scales.Évora, 8-9th May, 2006C. Cramez, Switzerlandccramez@compuserve.com
Geoscientists know a scale is necessary to interpretan outcrop or seismic line.Without scales, orientation and location (outside of the geological setting) and the geological interpretationof a seismic line is meaningless, because self-similarity. Indeed, a slope delta is similar to a continental slopeand to any offlap.Self-similarity = FractalÉvora, 8-9th May, 200633C. Cramez, Switzerlandccramez@compuserve.com
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C. Cramez, Switzerland

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