Maurice Dreyfuss; Essai d'interpretation du coefficient de subsidence. Bulletin de la Société Géologique de France ; S6-III (1-3): 205–213. doi: https://doi.org/10.2113/gssgfbull.S6-III.1-3.205
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From comparison of the subsidence and filling of a given basin, based on values obtained from the coefficient of subsidence, conditions of climate and deformation of adjacent land masses can be deduced. Conclusions are summed up in a table.
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