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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.
Tectonics ( IF 3.3 ) Pub Date : 2020-06-18 , DOI: 10.1029/2020tc006213 Gerardo Suárez 1 , Gema V. Caballero‐Jiménez 2 , David A. Novelo‐Casanova 1
中文翻译：
G.Suárez等人的评论“过去450年来历史地震证明的跨墨西哥火山带地壳活动变形”。
更新日期：2020-06-18
Tectonics ( IF 3.3 ) Pub Date : 2020-06-18 , DOI: 10.1029/2020tc006213 Gerardo Suárez 1 , Gema V. Caballero‐Jiménez 2 , David A. Novelo‐Casanova 1
Affiliation
- 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
中文翻译：
G.Suárez等人的评论“过去450年来历史地震证明的跨墨西哥火山带地壳活动变形”。
- 确定重要历史地震的震级和震中位置，反演大地震数据
- TMVB处于活动构造变形中，并且在几个已绘制的活动断层上发生了中型地震
- 在TMVB上发生地震的地方，没有映射的断层存在
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