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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1,087
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Cumulative views and downloads
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Total article views: 905 (including HTML, PDF, and XML)
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772
122
11
905
43
19
36
HTML: 772
PDF: 122
XML: 11
Total: 905
Supplement: 43
BibTeX: 19
EndNote: 36
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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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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: 1,087 (including HTML, PDF, and XML)
Thereof 1,046 with geography defined
and 41 with unknown origin.
Total article views: 905 (including HTML, PDF, and XML)
Thereof 873 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...