Surface and Subsurface Integration for the Mesozoic Rifting in the Eastern Cordillera, Colombia

• DOI: 10.3997/2214-4609.202012018
• Publication Date: 2021-01-15T16:16:53Z
• Authors: M. Reyes Correa; J. Kley; A. Mora
• Keywords: Foothills; Thrust fault

Summary The Eastern Cordillera is bounded by the Middle Magdalena Valley basin in west and Llanos Foothills to east. It commonly interpreted have grown from a Mesozoic rift that became inverted during Cenozoic Andean orogeny both eastern western margins of were thrust over adjacent basins inversion, resulting complex combination thick-skinned thin-skinned structures. geological evolution study area key understanding structural configuration related such as Valley. influence on geometry syn post – rift, has been only detected at levels below normal range seismic acquisition design, nevertheless, exposure units structures, allowing revisit collect stratigraphic data. In order correlate with subsurface data, timing kind fault displacements, implications MMV development. However, these methods provide constrained approach evolution, they require verification other tools as; date synrift U-Pb detect integrate it modeling.