Structural pattern of the Todos Santos Coastal Plain, based on geophysical data

Fuente: Redalyc · Ciencias Marinas

A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and air is used to integrate the structural framework and tectonic model of this area. The present work collected all the available data, homogenized them, and maintained them at their...

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Autor principal: Marco A. Pérez Flores
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Publicado: Universidad Autónoma de Baja California 2004
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author Marco A. Pérez Flores
author_facet Marco A. Pérez Flores
collection Ciencias Marinas
container_title Ciencias Marinas
contents Structural pattern of the Todos Santos Coastal Plain, based on geophysical data Marco A. Pérez Flores Luis A. Gallardo Delgado Antonio González Fernández Rogelio Vázquez Francisco Suárez Vidal Ciencias de la Tierra gravity structure magnetics coastal plain geophysical data A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and airis used to integrate the structural framework and tectonic model of this area. The present work collected all the available data,homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magneticdata from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesiticbasement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from thethree-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basinassociated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time. 2004 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48030208 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.2 Vol.30
ctrlnum oai:cienciasmarinas.com.mx:article/180
10.7773/cm.v30i2.180
description A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and air is used to integrate the structural framework and tectonic model of this area. The present work collected all the available data, homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magnetic data from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesitic basement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from the three-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basin associated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time. Se integró el marco estructural y el modelo tectónico de la Planicie Costera de Todos Santos, utilizando un conjunto de datos gravimétricos y magnéticos tomados entre 1962 y 2000 en tierra, aire y mar. En el presente trabajo se integró toda la información disponible, se homogeneizó y se mantuvo a su altitud original. Se empleó una nueva técnica de inversión conjunta de datos gravimétricos y magnéticos para estructuras tridimensionales. Como resultado se obtuvo un mapa topográfico del basamento granítico-andesítico, donde se visualizan rasgos geológicos desconocidos hasta este trabajo. Se hicieron algunas secciones a partir del modelo tridimensional, en los que se establece el patrón estructural de la Planicie Costera de Todos Santos, el cual es típico de una cuenca extensional (pull-apart basin) asociada con un frente de arco en un ambiente tectónico durante la subducción de la placa Farallón a final del Mesozoico y principios del Cenozoico.
format Artículo científico
id redalyc_48030208
institution Redalyc
Ciencias Marinas
language en
publishDate 2004
publisher Universidad Autónoma de Baja California
spelling Structural pattern of the Todos Santos Coastal Plain, based on geophysical data
Patrón estructural de la Planicie Costera de Todos Santos, con base en datos geofísicos
Pérez-Flores, MA
Suárez-Vidal, F
Gallardo-Delgado, LA
González-Fernández, A
Vázquez, R
structure
coastal plain
geophysical data
gravity
magnetics
estructura
planicie costera
datos geofísicos
gravimetría
magnetometría
A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and air is used to integrate the structural framework and tectonic model of this area. The present work collected all the available data, homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magnetic data from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesitic basement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from the three-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basin associated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time.
Se integró el marco estructural y el modelo tectónico de la Planicie Costera de Todos Santos, utilizando un conjunto de datos gravimétricos y magnéticos tomados entre 1962 y 2000 en tierra, aire y mar. En el presente trabajo se integró toda la información disponible, se homogeneizó y se mantuvo a su altitud original. Se empleó una nueva técnica de inversión conjunta de datos gravimétricos y magnéticos para estructuras tridimensionales. Como resultado se obtuvo un mapa topográfico del basamento granítico-andesítico, donde se visualizan rasgos geológicos desconocidos hasta este trabajo. Se hicieron algunas secciones a partir del modelo tridimensional, en los que se establece el patrón estructural de la Planicie Costera de Todos Santos, el cual es típico de una cuenca extensional (pull-apart basin) asociada con un frente de arco en un ambiente tectónico durante la subducción de la placa Farallón a final del Mesozoico y principios del Cenozoico.
Universidad Autónoma de Baja California, Instituto de Investigaciones Oceanológicas
2004-03-06
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Peer-reviewed Article
Artículo Arbitrado
application/pdf
https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/180
10.7773/cm.v30i2.180
Ciencias Marinas; Vol. 30 No. 2 (2004); 349-364
Ciencias Marinas; Vol. 30 Núm. 2 (2004); 349-364
2395-9053
0185-3880
eng
https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/180/155
['Redalyc']
redalyc_48030208
Structural pattern of the Todos Santos Coastal Plain, based on geophysical data
['Structural pattern of the Todos Santos Coastal Plain, based on geophysical data', 'Marco A. Pérez Flores', 'Ciencias de la Tierra', 'gravity', 'structure', 'magnetics', 'coastal plain', 'geophysical data', 'Structural pattern of the Todos Santos Coastal Plain, based on geophysical data Marco A. Pérez Flores Luis A. Gallardo Delgado Antonio González Fernández Rogelio Vázquez Francisco Suárez Vidal Ciencias de la Tierra gravity structure magnetics coastal plain geophysical data A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and airis used to integrate the structural framework and tectonic model of this area. The present work collected all the available data,homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magneticdata from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesiticbasement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from thethree-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basinassociated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time. 2004 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48030208 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.2 Vol.30']
['Marco A. Pérez Flores']
['Marco A. Pérez Flores']
['Artículo científico']
['2004']
['Universidad Autónoma de Baja California']
['en']
['Ciencias de la Tierra', 'gravity', 'structure', 'magnetics', 'coastal plain', 'geophysical data']
['https://www.redalyc.org/articulo.oa?id=48030208']
['Structural pattern of the Todos Santos Coastal Plain, based on geophysical data Marco A. Pérez Flores Luis A. Gallardo Delgado Antonio González Fernández Rogelio Vázquez Francisco Suárez Vidal Ciencias de la Tierra gravity structure magnetics coastal plain geophysical data A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and airis used to integrate the structural framework and tectonic model of this area. The present work collected all the available data,homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magneticdata from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesiticbasement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from thethree-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basinassociated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time. 2004 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48030208 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.2 Vol.30']
spellingShingle Structural pattern of the Todos Santos Coastal Plain, based on geophysical data
Marco A. Pérez Flores
Ciencias de la Tierra
gravity
structure
magnetics
coastal plain
geophysical data
Structural pattern of the Todos Santos Coastal Plain, based on geophysical data Marco A. Pérez Flores Luis A. Gallardo Delgado Antonio González Fernández Rogelio Vázquez Francisco Suárez Vidal Ciencias de la Tierra gravity structure magnetics coastal plain geophysical data A set of gravity and magnetic data taken within the Todos Santos Coastal Plain between 1962 and 2000 from land, sea and airis used to integrate the structural framework and tectonic model of this area. The present work collected all the available data,homogenized them, and maintained them at their original altitude. A new technique of joint inversion for gravity and magneticdata from three-dimensional structures was applied. As a result, a well-defined topographic map of the granitic-andesiticbasement was obtained and previously unknown geological structures were depicted. Several cross-sections were made from thethree-dimensional model obtained, establishing the Todos Santos Coastal Plain structural pattern as a typical pull-apart basinassociated with a tectonic fore-arc during the subduction of the Farallón Plate in Late Mesozoic and Early Cenozoic time. 2004 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48030208 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.2 Vol.30
title Structural pattern of the Todos Santos Coastal Plain, based on geophysical data
title_alt Patrón estructural de la Planicie Costera de Todos Santos, con base en datos geofísicos
topic Ciencias de la Tierra
gravity
structure
magnetics
coastal plain
geophysical data
topic_facet structure
coastal plain
geophysical data
gravity
magnetics
estructura
planicie costera
datos geofísicos
gravimetría
magnetometría
url https://www.redalyc.org/articulo.oa?id=48030208
https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/180