@inproceedings{fdi:010012915,
  title = {{A}nalisis fractal de los tepetates},
  author = {{O}leschko, {K}. and {M}iranda, {M}.{E}. and {P}rat, {C}hristian},
  editor = {},
  language = {{SPA}},
  abstract = {{T}he degree of fragmentation and irregularity of tepetate areas can be measured with fractal parameters. {A} lot of different empirical fractal dimensions can be used with this purposed. {S}ome of these dimensions were estimated and compared in the present work. {T}he tepetates lineal and mass fractal dimensions were independent of the scale of measurement. {T}hese data indicate the near ideal fractal dimensionality of tepetate areas. {T}he doble value of lineal fractal dimension was similar to the mass fractal dimension. {T}he tepetate surface fractal dimensions indicate the considerable irregularities of tepetate areas boundaries related with advanced erosion in the studied area. ({R}{\'e}sum{\'e} d'auteur)},
  keywords = {{SOL} ; {EROSION} ; {METHODE} {D}'{ANALYSE} ; {CARTE} ; {FRACTAL} ; {SOL} {VOLCANIQUE} {INDURE} ; {TEPETATE} ; {MEXIQUE}},
  numero = {},
  pages = {90--97},
  booktitle = {{S}uelos volcanicos endurecidos},
  year = {1997},
  URL = {https://www.documentation.ird.fr/hor/fdi:010012915},
}