Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region

Located in the heart of the Bolivian orocline, the Cochabamba department and its two million inhabitants are exposed to frequent seismic activity. However, the tectonic structures causing these earthquakes remain poorly identified. Indeed, Bolivia’s national seismological network does not optimally...

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Main Authors: Gonzalo Antonio Fernandez M, Benoit Derode, Laurent Bollinger, Bertrand Delouis, Mayra Nieto, Felipe Condori, Nathan Sarret, Jean Letort, Stephanie Godey, Mathilde Wimez, Teddy Griffiths, Walter Arce
Format: Article
Language:English
Published: McGill University 2025-01-01
Series:Seismica
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Online Access:https://seismica.library.mcgill.ca/article/view/1380
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author Gonzalo Antonio Fernandez M
Benoit Derode
Laurent Bollinger
Bertrand Delouis
Mayra Nieto
Felipe Condori
Nathan Sarret
Jean Letort
Stephanie Godey
Mathilde Wimez
Teddy Griffiths
Walter Arce
author_facet Gonzalo Antonio Fernandez M
Benoit Derode
Laurent Bollinger
Bertrand Delouis
Mayra Nieto
Felipe Condori
Nathan Sarret
Jean Letort
Stephanie Godey
Mathilde Wimez
Teddy Griffiths
Walter Arce
author_sort Gonzalo Antonio Fernandez M
collection DOAJ
description Located in the heart of the Bolivian orocline, the Cochabamba department and its two million inhabitants are exposed to frequent seismic activity. However, the tectonic structures causing these earthquakes remain poorly identified. Indeed, Bolivia’s national seismological network does not optimally cover the area and the hypocentral locations of local earthquakes are therefore subject to large uncertainties which hinder their association with specific faults. We established a regional network consisting of 11 broadband and short-period seismic stations, spaced approximately 20 km apart. This study highlights the initial 6-month seismic bulletin made by manual and automated deep-neural-network based seismic phase picking. We also test the network's ability to resolve focal mechanisms of moderate to small events with a combined inversion of waveforms and polarities. Our preliminary results document midcrustal microseismicity located in the Main Thrust fault shear zone, and in its hangingwall, in a region affected by tectonic slivers and transverse faults impacting the sedimentary cover. These outcomes provide fresh insights into the fault system’s seismogenic behavior and potential across the Bolivian orocline.
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spelling doaj-art-d7bf55497e7f47b5a99b00a0ce99246f2025-01-29T17:24:07ZengMcGill UniversitySeismica2816-93872025-01-014110.26443/seismica.v4i1.1380Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba regionGonzalo Antonio Fernandez M0Benoit Derode1Laurent Bollinger2Bertrand Delouis3Mayra Nieto4Felipe Condori5Nathan Sarret6Jean Letort7Stephanie Godey8Mathilde Wimez9Teddy Griffiths10Walter Arce11Observatorio San Calixto, La Paz, BoliviaEOST, ITES, CNRS UMR 7063, Université de Strasbourg, Strasbourg, France, CEA, DIF, F-91297, Arpajon, France, Observatoire Midi Pyrénées, IRAP, CNRS UMR 5277, Université Paul Sabatier, Toulouse, France CEA, DIF, F-91297, Arpajon, France Géoazur, CNRS UMR 7329, Université Côte d'Azur, France Observatorio San Calixto, La Paz, BoliviaObservatorio San Calixto, La Paz, BoliviaCEA, DIF, F-91297, Arpajon, FranceObservatoire Midi Pyrénées, IRAP, CNRS UMR 5277, Université Paul Sabatier, Toulouse, France CEA, DIF, F-91297, Arpajon, FranceCEA, DIF, F-91297, Arpajon, FranceObservatorio San Calixto, La Paz, BoliviaObservatorio San Calixto, La Paz, BoliviaLocated in the heart of the Bolivian orocline, the Cochabamba department and its two million inhabitants are exposed to frequent seismic activity. However, the tectonic structures causing these earthquakes remain poorly identified. Indeed, Bolivia’s national seismological network does not optimally cover the area and the hypocentral locations of local earthquakes are therefore subject to large uncertainties which hinder their association with specific faults. We established a regional network consisting of 11 broadband and short-period seismic stations, spaced approximately 20 km apart. This study highlights the initial 6-month seismic bulletin made by manual and automated deep-neural-network based seismic phase picking. We also test the network's ability to resolve focal mechanisms of moderate to small events with a combined inversion of waveforms and polarities. Our preliminary results document midcrustal microseismicity located in the Main Thrust fault shear zone, and in its hangingwall, in a region affected by tectonic slivers and transverse faults impacting the sedimentary cover. These outcomes provide fresh insights into the fault system’s seismogenic behavior and potential across the Bolivian orocline. https://seismica.library.mcgill.ca/article/view/1380BoliviaOroclinemoment tensorautomated workflowAndes
spellingShingle Gonzalo Antonio Fernandez M
Benoit Derode
Laurent Bollinger
Bertrand Delouis
Mayra Nieto
Felipe Condori
Nathan Sarret
Jean Letort
Stephanie Godey
Mathilde Wimez
Teddy Griffiths
Walter Arce
Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
Seismica
BoliviaOrocline
moment tensor
automated workflow
Andes
title Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
title_full Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
title_fullStr Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
title_full_unstemmed Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
title_short Unveiling midcrustal seismic activity at the front of the Bolivian altiplano, Cochabamba region
title_sort unveiling midcrustal seismic activity at the front of the bolivian altiplano cochabamba region
topic BoliviaOrocline
moment tensor
automated workflow
Andes
url https://seismica.library.mcgill.ca/article/view/1380
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