Geochemical Characterization of the Paleocene Ewekoro Limestone Formation, SW Nigeria: Implications for Provenance, Diagenesis and Depositional Environment
Geochemical Characterization of the Paleocene Ewekoro Limestone Formation, SW Nigeria: Implications for Provenance, Diagenesis and Depositional Environment作者机构：Department of Geology University of Ibadan Ibadan Nigeria Department of Geology Delta State University Abraka Nigeria
出 版 物：《Geomaterials》 (地质材料（英文）)
年 卷 期：2016年第6卷第3期
页 面：61-77页
学科分类：070902[理学-地球化学] 0709[理学-地质学] 07[理学]
主 题：Geochemical Characterization Ewekoro Formation Ca/Mg Ratio Limestone Carbonate Silica
摘 要：The usefulness of limestone as an industrial raw material is dependent on the level of its purity, largely controlled by diagenesis and the depositional setting. Limestone samples (83) obtained from the Ewekoro Formation exposed in quarry sections at Shagamu were analyzed using X-Ray Fluorescence spectrometry (XRF). A geochemical characterization of result was done to evaluate the purity levels and the implications on provenance, diagenesis, and depositional setting of the limestone. Five limestone beds from quarry sections (15 locations) were logged. Beds “E, “D, “C, “B, and “A comprised sandy algal in sparry calcite cement, sandy biomicrite, algal biomicrite, sandy algal biomicrite, and the intra-sparite facies respectively. Results of major elements che- mistry indicated concentrations (in wt%) as follows: CaO (33.71 - 59.99), MgO (0.39 - 3.15), Al2O3 (0.47 - 3.23), Fe2O3 (0.51 - 3.43), SiO2 (0.47 - 45.98), SO3 (0.10 - 2.27), K2O (0.02 - 0.28), Na2O (0.00 - 10.0), TiO2 (0.00 - 0.27), P2O5 (0.02 - 0.92), MnO (0.01 - 0.06) and Loss on ignition (17.64 - 45.20). Geochemical result showed that the samples are enriched in CaO, while SiO2 varies widely, likely due to hinterland input. Plots of SiO2 versus CaO concentrations depicted a negative correlation attributable to chemical diagenetic processes. Diagenesis of the carbonate in form of reversible replacement of SiO2 with CaO and vice versa occurred under a shallow marine condition. This negative correlation between these oxides (CaO and SiO2) dictates zones of high purity limestones that are of desirable industrial applications. Relatively high silica content in the northwestern part is possible indication of outlets to the continental or inland areas where clastic sediment source may have been prominent. Ratios of Ca/Mg and Mg/Ca indicated a relati
维普期刊数据库