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- W202671535 abstract "The structural evolution of the Maracaibo basin shows a series of complex tectonic events: extension transtension (early Eocene and middle Eocene), caused by oblique convergence in South America and the Caribbean plates, as well as a tectonic inversion during the late Eocene and Pliocene ages. The main objective of this research is to perform a structural model in the Atico Region, basin of Maracaibo Lake, to contributes in the static model for future exploitation plans. The Atico region is located in block I, in the north-central part of the Maracaibo basin. Geologically, this is limited between two erosive surfaces recognized at regional level (discordance of the Paleocene and Eocene unconformity). From the structural point of view, the Atico is an elongated block with NE-SW direction limited by the Lama-Icotea fault to the West and the Atico fault to the East with reverse behavior, that verge against Lama-Icotea in depth towards the West. This block is divided internally by faults Intra-Atico oriented NE-SW, interpreted in seismic like a reverse behavior and structural closure at depth within the Misoa formation. The Lama-Icotea fault constitutes the most important structural element of block I, oriented N15 ° E, strike-slip siniestral fault results a compressive-transpressive tectonics and distensive-transtensive product that affected it during the Mesozoic and Cenozoic ages, which developed structures like the Atico in a process of structural invesion. The origin of the Atico block in base of information in this research is related to a late stage of shortening of block compression-transpresion, allowing the partial expulsion of the prism that is restricted to the Lama-Icotea fault and the Atico fault representing a pop structure broked to up and compressed towards their base." @default.
- W202671535 created "2016-06-24" @default.
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- W202671535 date "2014-01-01" @default.
- W202671535 modified "2023-09-27" @default.
- W202671535 title "Evidencias de Inversión Estructural a partir del reconocimiento de estructuras del tipo “Pop Up” a lo largo de la falla transcurrente Lama-Icotea, en la Región de Ático, Cuenca de Maracaibo, Venezuela" @default.
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