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- W2137482011 abstract "The subduction erosion model recently proposed as an explanation for the Cenozoic truncation of southern Mexico is confronted with the traditional model by detachment of the Chortis block. The Chortis block detachment model has some objections previously recognized. In this work, the main objections arisen from the geometric array of the Polochic-Motagua fault system are resolved with a relative left lateral slip of ca. 120 km between the Chiapas Massif and the Polochic-Motagua system, along a southeasterly trend. Such displacement is inferred from the active shear deformation on the Chiapas region and from structural features on the platform of the Gulf of Tehuantepec. On the basis of the geologic record of southern Mexico, with emphasis on mesozoic basins, as well as on the Chortis block stratigraphic record, the model of Cenozoic tectonic truncation of southern Mexico by detachment of Chortis block and its transference to the Caribbean plate is favored. We discard subduction erosion as the process that trimmed southern Mexico, because its invocation implies a subduction erosion rate of 823.5 km 3 /m.y./km, a rate 20 times greater than the fast subduction erosion presently occurring. Detachment of the Chortis block remains as the more plausible model for the Cenozoic tectonic reduction of southern Mexico." @default.
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- W2137482011 date "2009-04-01" @default.
- W2137482011 modified "2023-10-01" @default.
- W2137482011 title "Evaluación geológica de los modelos para el truncamiento cenozoico del sur de México: Erosión por subducción y detachment del bloque Chortís" @default.
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