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When too few field measurements are available for the geological mod-ling of complex folded structures, results of implicit methods typically exhibit an unsatisfactory bubbly aspect. However, in such cases, anisotropy data are often readily available but not fully exploited. Among them, fold axis data are a straightforward indicator of this local anisotropy direction. Focusing on the so-called potential field method, this work aims to evaluate the effect of the incorporation of such data intodoi:10.21203/rs.3.rs-485111/v1 fatcat:w2uu7xkhz5fzrn5562hqzw6s7u