Abstract
Maria Ines Oeste, an oil and gas field in Argentina's Magallanes Foreland Basin (also called Austral Basin) produces from Maria Inees sandstones that are known to represent the base of a second order transgressive system tract (TST), deposited during Late Maastrichtian times in a coastal to open shelf environment. Figure 1 outlines the basic tectonic framework of the Austral Basin.
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