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: 1,284 (including HTML, PDF, and XML)
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1,091
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1,284
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HTML: 1,091
PDF: 173
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Total: 1,284
Supplement: 61
BibTeX: 30
EndNote: 62
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Cumulative views and downloads
(calculated since 04 Jul 2024)
Total article views: 1,102 (including HTML, PDF, and XML)
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909
173
20
1,102
61
30
62
HTML: 909
PDF: 173
XML: 20
Total: 1,102
Supplement: 61
BibTeX: 30
EndNote: 62
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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Total: 182
BibTeX: 0
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Views and downloads (calculated since 04 Jul 2024)
Cumulative views and downloads
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Viewed (geographical distribution)
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: 1,284 (including HTML, PDF, and XML)
Thereof 1,231 with geography defined
and 53 with unknown origin.
Total article views: 1,102 (including HTML, PDF, and XML)
Thereof 1,058 with geography defined
and 44 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...