Sismicidad Superlicial en Consata - Mapiri, Altiplano Norte de La paz

A.J. Vega B.

doi:10.3997/2214-4609-pdb.316.105

Sismicidad Superlicial en Consata - Mapiri, Altiplano Norte de La paz
By A.J. Vega B.
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 2nd International Congress of the Brazilian Geophysical Society, Oct 1991, cp-316-00105
DOI: https://doi.org/10.3997/2214-4609-pdb.316.105

Abstract

El Altiplano de Bolivia con una altura en promedio de 3800 metros se extiende entre las Cordilleras Occidental y Oriental de Los Andes, figura 1, formando un gráven delimitado al Oeste por la falla-lineamiento Huancarani y al Este por la falla Uyuni-Poopo, y una serie de fallas paralelas de dirección Andina (Claure, 1983). En esta plataforma de un espesor considerable, 15 km de materiales del cretácico y terciario (Newell, 1949), la actividad sismica es notoriamente de profundidad intermedia (70 a 300 km) relacionada con la subducción de la Placa de Nazca.

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1991-10-28

2024-04-25

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Sismicidad Superlicial en Consata - Mapiri, Altiplano Norte de La paz

Abstract

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The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture