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Part 1: Document Description
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Citation |
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Title: |
Copiapó_Experiment_Catalogue |
Identification Number: |
doi:10.34691/FK2/91GHJE |
Distributor: |
Repositorio de datos de investigación de la Universidad de Chile |
Date of Distribution: |
2022-01-20 |
Version: |
2 |
Bibliographic Citation: |
Pastén, Francisco, 2022, "Copiapó_Experiment_Catalogue", https://doi.org/10.34691/FK2/91GHJE, Repositorio de datos de investigación de la Universidad de Chile, V2, UNF:6:EqHO6fRB2jndKVp7ubQlqQ== [fileUNF] |
Citation |
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Title: |
Copiapó_Experiment_Catalogue |
Identification Number: |
doi:10.34691/FK2/91GHJE |
Authoring Entity: |
Pastén, Francisco (Universidad de Chile) |
Distributor: |
Repositorio de datos de investigación de la Universidad de Chile |
Access Authority: |
Pastén, Francisco |
Access Authority: |
Potin, Bertrand |
Access Authority: |
Azúa, Kellen |
Access Authority: |
Ruiz, Sergio |
Depositor: |
Pastén, Francisco |
Date of Deposit: |
2021-10-09 |
Holdings Information: |
https://doi.org/10.34691/FK2/91GHJE |
Study Scope |
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Keywords: |
Earth and Environmental Sciences, Sismicidad |
Abstract: |
The subduction of different features such as oceanic ridges, fractures zones or seamounts are important for the accurate characterization of subduction zones. These structures may affect the along-dip variability of seismic behavior and eventually trigger slow earthquakes. Here we studied the along- dip influence of the Copiapó ridge subduction in the Atacama region, North-Central Chile, an area where seismic swarms, low coupling values and slow earthquakes have been reported. We built a seismic catalog including repeating earthquakes and non-volcanic tremors (NVT), and performed a 3-D tomography for P-wave velocity and Vp/Vs ratio. We identify along-dip segmentation involving 4 distinct segments: (1) a locked seismogenic zone (20 to 35 km depth), hosting ordinary clustered micro-seismicity and repeating earthquakes; (2) a transition zone (35 to 42 km) with non-volcanic tremor and low seismicity; (3) a zone (42 to 60 km) without seismicity and with slow-slip events and (4) a deep zone with more abundant seismicity. The velocity models show differences among these zones: while low velocity anomalies of Vp and Vs, and Vp/Vs ratio between 1.76 and 1.82 are observed in the deep zone, higher velocities are present in the other areas. These features indicate that SSE are located in a zone with higher pore fluid pressure. We propose that these geodynamic differences are generated by the subduction of heterogenic seamounts associated to the Copiapó ridge. |
Notes: |
Se recomiendo utilizar el programa Generic Mapping Tool (GMT) para la visualización de los datos. |
Methodology and Processing |
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Data Access |
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Other Study Description Materials |
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File Description--f497 |
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File: NVTs.tab |
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Label: |
Cluster_Similar_Events_Catalog.txt |
Notes: |
text/plain |
Label: |
Copiapo_Experiement_catalogue.txt.txt |
Notes: |
text/plain |
Label: |
NVTs_Catalog.txt |
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text/plain |
Label: |
data_Copiapo_autoPicks.insl |
Notes: |
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Label: |
data_Copiapo_manuPicks.insl |
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Label: |
stations_Copiapo.sta |
Notes: |
application/octet-stream |