The Guayape-Papalutla fault system: A continuous Cretaceous structure from southern Mexico to the Chortis block? Tectonic implications: COMMENT and REPLY: COMMENT

Abstract

The use of piercing points in making paleogeographic reconstructions greatly adds to their accuracy beyond that available using other techniques. Thus, [Silva-Romo's (2008)][1] proposal that the Papalutla fault in southern Mexico and the Guayape fault in Honduras provide piercing points to constrain