Stratigraphic and petrographic study of the limestones of the La Tomita sector, in the municipality of Manaure-Cesar, Colombia

• Main Authors: De Los Reyes Díaz, Génesis Carolina, Mendoza Mejía, Zamir, Mosquera Nieves, Eloy I., Rojas Martínez, Elías Ernesto, Manco Jaraba, Dino Carmelo, Lascarro Navarro, Frank
• Format: Article in Journal/Newspaper
• Language: English; Spanish
• Published: Universidad de la Costa CUC 2022
• Subjects: Caliza; Estratigrafía; Manaure; Petrografía; Limestone; Stratigraphy; Petrography; Shales; Cogollo; Planktonic foraminifera
• Online Access: https://revistascientificas.cuc.edu.co/ingecuc/article/view/2710

Introduction: In the La Tomita sector, municipality of Manaure (Cesar), outcrop a stratigraphic sequence of biomicrite limestones, biopelmicrites, pelmicrites, wackestones and packstones intercalated with shales, corresponding to the Lagunita Formation of the Cogollo Group. Objective: To know the stratigraphic aspects, mineralogical composition and paleoenvironmental conditions of the outcropping limestones. Methodology: It proceeded with a lithostratigraphic description in the massif and taking samples in situ, twelve samples were extracted, of which seven were taken for petrographic analysis. Results: Wackestone facies with pelagic microfossils, bioclastic packstone, wackestone with worn mollusc bioclasts and wackestone with peloids were recognized. Petrographically, the limestones in this sector are made up of zircon, glauconite, sparite, micrite, pellets, planktonic foraminifera of the genus Heterohelix, of the Moremani species, and foraminifera of the genus Hedbergella and Trocoidea species. Bivalve fossils and some algae were also observed. Conclusions: These facies allowed establishing that these limestones were formed in an environment of medium platform with some external platform intervals, covering an area of facies of open sea. Introducción: En el sector La Tomita, municipio de Manaure (Cesar), aflora una secuencia estratigráfica de calizas biomicritas, biopelmicritas, pelmicritas, tipo wackestone y packstone intercalados con shales, correspondientes a la Formación Lagunita del Grupo Cogollo. Objetivo: Conocer los aspectos estratigráficos, composición mineralógica y condiciones paleoambientales de las calizas aflorantes Metodología: se procedió con una descripción litoestratigráfica en el macizo y toma de muestras in situ. Se extrajeron doce muestras, de la cuales se tomaron siete para análisis petrográfico. Resultados: Se reconocieron facies de wackestone con microfósiles pelágicos, packstone bioclásticos, wackestone con bioclastos de moluscos desgastados y wackestone con peloides; ...