Dipartimento di Geoscienze, Università degli Studi di Padova, Padua, Italy
Sezione di Roma 1, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
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Total article views: 1,105 (including HTML, PDF, and XML)
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967
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12
1,105
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38
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PDF: 126
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Supplement: 45
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Cumulative views and downloads
(calculated since 04 Jul 2024)
Total article views: 923 (including HTML, PDF, and XML)
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785
126
12
923
45
20
38
HTML: 785
PDF: 126
XML: 12
Total: 923
Supplement: 45
BibTeX: 20
EndNote: 38
Views and downloads (calculated since 14 Jan 2025)
Cumulative views and downloads
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Total article views: 182 (including HTML, PDF, and XML)
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182
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182
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Views and downloads (calculated since 04 Jul 2024)
Cumulative views and downloads
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,105 (including HTML, PDF, and XML)
Thereof 1,064 with geography defined
and 41 with unknown origin.
Total article views: 923 (including HTML, PDF, and XML)
Thereof 891 with geography defined
and 32 with unknown origin.
Total article views: 182 (including HTML, PDF, and XML)
Thereof 173 with geography defined
and 9 with unknown origin.
We investigate an exhumed hydrothermal system in the Atacama Desert (Chile) to understand how earthquake swarms form. Wall rocks near fault veins experienced high-stress pulses, and fault veins underwent cyclic crack opening and shearing. These findings suggest ancient earthquake swarm activity, from dynamic crack propagation to repeated crack opening and shearing. This system represents a unique geological record of earthquake swarms, providing insights into their initiation and evolution.
We investigate an exhumed hydrothermal system in the Atacama Desert (Chile) to understand how...