尼日利亚尼日尔三角洲北部沉积带VIC 97井浅形态生物地层学

A. Asadu, V. O. Onowaro
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引用次数: 0

摘要

对位于尼日尔三角洲北部沉积带OML 38的VIC-97井的460 ~ 4550英尺的60个沟切岩样品进行了孢粉学和沉积学研究,以确定岩相单元和岩石演为的年龄。孢粉样品分析的标准方法被用于从岩石基质中分解孢粉。以割沟岩样的测井特征、砂泥比、结构属性、矿物成分等为岩性参数,建立了两个岩相单元;过渡性单元砂泥比为80:20,大陆单元砂泥比为98:2,分别属于上Agbada组和Benin组。孢粉学分析表明,检索到的孢粉形态数量众多,且具有合理的多样性,特别是在样本区间的下部。孢粉带的划分基于孢粉花的重要种类组合及其地层分布。根据第一次和最后一次在井下出现的情况,识别出13个非正式生物带,并与p560、P580和P624进行比较,确定了研究层段的早至晚渐新世年龄。
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Palynomorph Biostratigraphy of VIC 97 Well, Nothern Depo Belt, Niger Delta, Nigeria
Palynological and sedimentological studies were conducted on sixty ditch cutting rock samples from interval 460 to 4550 feets of VIC-97 well, located at OML 38, Northern Depo-belt, Niger-Delta, to delineate lithofacies units and the age of the rock succession. Standard methods of palynological sample analysis were used to disaggregate the palynomorphs from the rock matrix. Log signatures, sand/shale ratios, textural attributes, and accessory mineal compositions of ditch cutting rock samples were used as lithologic parameters to establish two lithofacies units; the transitional unit having a sand/shale ratio of 80:20 and the continental Unit having a 98:2 ratio ascribed to upper Agbada and Benin formation respectively. Palynological analysis revealed that the retrieved palynomorphs were numerous and reasonably diversified, particularly in the lower portion of the sample interval. Palynological zonation was based on the palynofloral assemblage of important species and their stratigraphic distribution. Thirteen informal biozones were recognised on the basis of their first and last downhole occurences and compared with P 560, P580 and P624 to delineate an early to late Oligocene age for the studied interval.
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