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sediments; these marine cenozoic depositions were originally defined as Tampico-Misantla<br />
Basin by López-Ramos (1956).<br />
The ongoing uplift of the SMO left very narrow coastal plains and continental shelves,<br />
hence the coastal systems would go from a prodelta to a slope, and where the transport of<br />
sediments by means of turbidity currents prevailed, there would be flow of debris and<br />
landslides, which would produce deposition of submarine fans at the bottom of the<br />
seafloor (basin), overlapping each other and generating submarine erosion during their<br />
development.<br />
By the end of the Cenozoic, deltaic environments prevailed.<br />
Tuxpan<br />
Poza Rica<br />
Tecolutla<br />
Tertiary Sedimentary model (Paleogene and Neogene). Note that delta environments<br />
were deposited above the Chicontepec formation<br />
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