Open AccessThe Guayape-Papalutla fault system: A continuous Cretaceous structure from southern Mexico to the Chortis block? Tectonic implications: COMMENT and REPLY: REPLY
Author(s) -
Gilberto Silva-Romo
Publication year - 2008
Publication title -
geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.609
H-Index - 215
eISSN - 1943-2682
pISSN - 0091-7613
DOI - 10.1130/g25152y.1
Subject(s) - geology , cretaceous , block (permutation group theory) , fault (geology) , tectonics , seismology , paleontology , geometry , mathematics
In [Figure 1][1] of his Comment ([Keppie, 2008][2]), Keppie confused the Papalutla fault with the Teloloapan fault in his Comment's Figure. Here (in my [Figure 1][1]), I correctly identify the Papalutla fault in south Mexico, which supports my original hypothesis (Silva-Romo, 2008).![Figure 1][3
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