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Reply to Comment on “Active Crustal Deformation in the Trans‐Mexican Volcanic Belt as Evidenced by Historical Earthquakes During the Last 450 Years” by G. Suárez et al.
Author(s) -
Suárez Gerardo,
CaballeroJiménez Gema V.,
NoveloCasanova David A.
Publication year - 2020
Publication title -
tectonics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.465
H-Index - 134
eISSN - 1944-9194
pISSN - 0278-7407
DOI - 10.1029/2020tc006213
Subject(s) - geology , seismology , volcanic belt , volcano , tectonics , deformation (meteorology) , active fault , volcanic rock , oceanography
Key Points The magnitude and epicentral locations important historical earthquakes are determined inverting the macroseismic data The TMVB is under active tectonic deformation and moderate‐sized earthquakes occur on several mapped active faults Earthquakes have occurred on the TMVB in areas where no mapped faults exist