Chemostratigraphy of the Cretaceous Yolde Formation in Yola Sub-Basin, Northern Benue Trough, Ne Nigeria

Ahmad Fauziyah Rufai, K. S. Nuhu, A. Maigari, Boniface Finthan
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Abstract

This research aims to determine the chemostratigraphy of the Yolde Formation. The formation has been inadequately studied  systematically in the light of chemostratigraphy. The existing works on the formation either lack representativeness in terms of the  proxies used or are subjective during their division procedures. From the field studies, five (5) samples of sandstone and shale units of  the Yolde Formation were collected. The samples were analyzed for both major and trace elements using an X-ray fluorescence machine.  The following geochemical parameters were studied; Al2O3, Al2O3/Fe2O3, KO2/Al2O3, TiO2/Al2O3, CaO, Cr, Rb/Sc, and Zr. From the studies,  six (6) chemozones were identified in the Yolde Formation. Transgressive and regressive depositional sequences were observed  with a significant sequence boundary of maximum flooding surface which is a time-significant feature. The chemostratigraphic scheme  could not only be comparable to the regional sequence stratigraphic scheme but also more objective and higher resolution. This research  gives a systematic chemostratigraphic analysis of Yolde Formation, which testifies to the feasibility and potential of the usage of  chemostratigraphy for stratigraphic development. 
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尼日利亚内贝努埃海槽北部约拉次盆地白垩纪约尔德地层的化合地层学
这项研究旨在确定约尔德地层的化合地层学。从化学地层学的角度来看,对该地层的系统研究还很不够。现有关于该地层的研究要么在使用的代用指标方面缺乏代表性,要么在划分过程中存在主观性。在实地研究中,采集了五(5)个约尔德地层砂岩和页岩单元样本。使用 X 射线荧光仪对样本进行了主要元素和微量元素分析。 研究了以下地球化学参数:Al2O3、Al2O3/Fe2O3、KO2/Al2O3、TiO2/Al2O3、CaO、Cr、Rb/Sc 和 Zr。通过研究,在约尔德地层中发现了六(6)个化合区。观察到了递变和回归沉积序列,其中最大洪积面是一个重要的序列边界,这是一个具有时间意义的特征。化合地层方案不仅可以与区域层序地层方案相媲美,而且更加客观,分辨率更高。该研究对约尔德地层进行了系统的化学地层学分析,证明了化学地层学在地层发展中应用的可行性和潜力。
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