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Les différentes populations de granis des agrégats polycristallins monominéraux déformés et cristallises sont classés suivant leur forme d'après le diagramme de blaschke. On étudie les polyèdres trivalents à 13 et 14 faces grâces a un logiciel de calcul des coordonnées des sommets. On peut aussi déduire les caractéristiques d'un polyèdre a partir de ses coordonnées ainsi que des simulations numériques d'intercepts linéaires et planauss du polyèdre isole et de l'agrégat qu'il engendre s'il est empilable

Principes de stéréologie des formes en pétrographie quantitative