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After a severe M W 5.7 earthquake on October 17, 2015 in El Galpón in the province of Salta NW Argentina, I installed a local seismological network around the estimated epicenter. The network covered an area characterized by inherited Cretaceous normal faults and neotectonic faults with unknown recurrence intervals, some of which may have been reactivated normal faults. The 13 three-component seismic stations recorded data continuously for 15 months. The 2015 earthquake took place in the Santa Bárbara System of the Andean foreland, at about 17km depth. This region is the easternmost morphostructural region of the central Andes. As a part of the broken foreland, it is bounded to the north by the Subandes fold-and-thrust belt and the Sierras Pampeanas to the south; to the east lies the Chaco-Paraná basin. A multi-stage morphotectonic evolution with thick-skinned basement uplift and coeval thin-skinned deformation in the intermontane basins is suggested for the study area. The release of stresses associated with the foreland ...
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Dissertation Universität Potsdam 2020
Weitere Ausg.:
Erscheint auch als Druck-Ausgabe Zeckra, Martin Seismological and seismotectonic analysis of the northwestern Argentine Central Andean foreland Potsdam, 2020
Sprache:
Englisch
Schlagwort(e):
Provinz Salta
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Erdbeben
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Vorland
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Seismotektonik
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Störung
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Neotektonik
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Argentinien
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Zentralanden
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Seismologie
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Erdbebenzone
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Seismometrie
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Orientierung
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Tektonik
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Provinz Salta
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Datenauswertung
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Deformation
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Erdbebenherd
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Hochschulschrift
DOI:
10.25932/publishup-47324
URN:
urn:nbn:de:kobv:517-opus4-473240
URL:
https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-473240
URL:
https://d-nb.info/1219579378/34
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