Broad depth range seismic imaging of the subducted Nazca Slab, North Chile

Buske, S.; Lüth, S.; Meyer, H.; Patzig, R.; Reichert, C.; Shapiro, S.; Wigger, P.; Yoon, M.

doi:10.1016/S0040-1951(02)00117-8

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Broad depth range seismic imaging of the subducted Nazca Slab, North Chile

Authors

Buske, S.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Lüth, S.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Meyer, H.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Patzig, R.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Reichert, C.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Shapiro, S.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Wigger, P.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Yoon, M.
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

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Citation

Buske, S., Lüth, S., Meyer, H., Patzig, R., Reichert, C., Shapiro, S., Wigger, P., Yoon, M. (2002): Broad depth range seismic imaging of the subducted Nazca Slab, North Chile. - Tectonophysics, 350, 4, 273-282.
https://doi.org/10.1016/S0040-1951(02)00117-8

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_61237

Abstract

In this paper, we present a compilation of modern seismic and seismological methods applied to image the subduction process in North Chile, South America. We use data from active and passive seismic experiments that were acquired within the framework of the German Collaborative Research Center SFB267 ‘Deformation Processes in the Andes’. The investigation area is located between 20° and 25°S and extends from the trench down to 100 km depth. In the depth range between the sea bottom and 15 km, we process an offshore seismic reflection profile using a recently developed velocity-model-independent stacking procedure. We find that the upper part of the subducting oceanic lithosphere in this depth range is characterized by a horst-and-graben structure. This structure supports an approximately 3 km thick coupling zone between the plates. In the depth range between 15 and 45 km, we analyse the spatial distribution of aftershocks of the Antofagasta earthquake (1995). The aftershock hypocenters are concentrated in an approximately 3 km thick layer. Finally, in the depth range between 45 and 100 km, we apply Kirchhoff prestack depth migration to the onshore ANCORP profile. A double reflection zone is observed between 45 and 60 km depth, which may represent the upper and lower boundary of the subducted oceanic crust. Over the whole range down to more than 80–90 km depth, we obtain an image of the subducting slab. At that depth, the hypocenters of local earthquakes deviate significantly in the direction perpendicular to the slab face from the reflective parts of the slab. Consequently, our results yield a complete seismic image of the downgoing plate and the associated seismic coupling zone.