![](http://satori.geociencias.unam.mx/public/journals/1/cover_issue_110_en_US.jpg)
Cover image:
Cupidito exposed as a transgressive unit at the south limb of Los Muertos anticline in the emblematic locality of La Huasteca, Nuevo Leon. Peritidal carbonates from the Cupido Formation, organized in subvertical strata, represent a marine regression that developed a sequence boundary marked by a collapse breccia (central vertical wall). See Torres de la Cruz et al. in this issue.
Published:
2020-03-31