Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico

The continuous reflection seismic profiles that are available of the onshore California continental borderland, between Punta Banda and Punta Santo Tomás, B.C., show a series of basins and topographical heights with a similar direction as the fault systems located in the continental region. From th...

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Main Authors: R Moldrano-Salgado, V Wong-Ortega
Format: Article
Language:English
Published: Universidad Autónoma de Baja California 1991-03-01
Series:Ciencias Marinas
Online Access:http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/779
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author R Moldrano-Salgado
V Wong-Ortega
author_facet R Moldrano-Salgado
V Wong-Ortega
author_sort R Moldrano-Salgado
collection DOAJ
description The continuous reflection seismic profiles that are available of the onshore California continental borderland, between Punta Banda and Punta Santo Tomás, B.C., show a series of basins and topographical heights with a similar direction as the fault systems located in the continental region. From the analysis of these profiles, it has been possible to determine the marine expression of the Bahía Soledad fault zone, which mainly affects the sedimentary deposits of the Ensenada basin. Furthermore, evidence was found of extensional processes, such as negative flower structures associated to the main line of the San Isidro fault. From this, we infer that the study area is controlled by tectonic processes caused by the strike-slip fault systems located in the area and that are generally consistent with a right-lateral fault model characteristic of a region subjected to tensional stress.
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spelling doaj.art-810f61f65a6f407385353689ad84dfb22024-03-04T16:44:10ZengUniversidad Autónoma de Baja CaliforniaCiencias Marinas0185-38802395-90531991-03-0117110.7773/cm.v17i1.779Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, MexicoR Moldrano-Salgado0V Wong-Ortega1Estación de Investigación Oceanográfica de EnsenadaCentro de Investigación Científica y de Educación Superior de Ensenada The continuous reflection seismic profiles that are available of the onshore California continental borderland, between Punta Banda and Punta Santo Tomás, B.C., show a series of basins and topographical heights with a similar direction as the fault systems located in the continental region. From the analysis of these profiles, it has been possible to determine the marine expression of the Bahía Soledad fault zone, which mainly affects the sedimentary deposits of the Ensenada basin. Furthermore, evidence was found of extensional processes, such as negative flower structures associated to the main line of the San Isidro fault. From this, we infer that the study area is controlled by tectonic processes caused by the strike-slip fault systems located in the area and that are generally consistent with a right-lateral fault model characteristic of a region subjected to tensional stress. http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/779
spellingShingle R Moldrano-Salgado
V Wong-Ortega
Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
Ciencias Marinas
title Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
title_full Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
title_fullStr Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
title_full_unstemmed Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
title_short Structural characteristics of the region between Punta Banda and Punta Santo Tomas, Baja California, Mexico
title_sort structural characteristics of the region between punta banda and punta santo tomas baja california mexico
url http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/779
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