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Se integro el marco estructural y el modelo tectonico de la Planicie Costera de Todos Santos, utilizando un conjunto de datos gravimetricos y magneticos tomados entre 1962 y 2000 en tierra, aire y mar. En el presente trabajo se integro toda la informacion disponible, se homogeneizo y se mantuvo a su altitud original. Se empleo una nueva tecnica de inversion conjunta de datos gravimetricos y magneticos para estructuras tridimensionales. Como resultado se obtuvo un mapa topografico del basamento granitico-andesitico, donde se visualizan rasgos geologicos desconocidos hasta este trabajo. Se hicieron algunas secciones a partir del modelo tridimensional, en los que se establece el patron estructural de la Planicie Costera de Todos Santos, el cual es tipico de una cuenca extensional (pull-apart basin) asociada con un frente de arco en un ambiente tectonico durante la subduccion de la placa Farallon a final del Mesozoico y principios del Cenozoico.  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 Farallon Plate in Late Mesozoic and Early Cenozoic time.

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