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: 2,621 (including HTML, PDF, and XML)
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2,258
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PDF: 295
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Total: 2,621
Supplement: 89
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EndNote: 82
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Cumulative views and downloads
(calculated since 04 Jul 2024)
Total article views: 1,518 (including HTML, PDF, and XML)
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1,163
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1,518
89
49
82
HTML: 1,163
PDF: 295
XML: 60
Total: 1,518
Supplement: 89
BibTeX: 49
EndNote: 82
Views and downloads (calculated since 14 Jan 2025)
Cumulative views and downloads
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Total article views: 1,103 (including HTML, PDF, and XML)
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1,095
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8
1,103
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Total: 1,103
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: 2,621 (including HTML, PDF, and XML)
Thereof 2,567 with geography defined
and 54 with unknown origin.
Total article views: 1,518 (including HTML, PDF, and XML)
Thereof 1,464 with geography defined
and 54 with unknown origin.
Total article views: 1,103 (including HTML, PDF, and XML)
Thereof 1,103 with geography defined
and 0 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...