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首页> 外文期刊>International Journal of Advanced Geosciences >Foraminiferal biostratigrpahy of oshi-13 field, coastal and central swamp depobelt, Niger delta basin, Nigeria
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Foraminiferal biostratigrpahy of oshi-13 field, coastal and central swamp depobelt, Niger delta basin, Nigeria

机译:尼日利亚尼日尔三角洲盆地沿海和中部沼泽沉积带的oshi-13田的有孔虫生物地层

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摘要

A high resolution Foraminiferal biostratigrpahic study has been carried out using data from three wells located in the Coastal and Central Swamp depobelts of Niger Delta. The study defined six (N6-N15) Foraminiferal zones for the early to middle Miocene Niger Delta on the basis of index Foraminiferal and this was correlated to Blow, 1969 and Bergreen et al., 1995. Foraminiferal analysis shows that Oshi-13 Field is very rich in calcareous and araneceous benthics, calcareous and planktic foraminiferal. The abudance of fossils and index fossils are responsible for constructing the biostratigraphic chart and hydrocarbon saturation in the field. The biostratigraphy chart constructed act as a basis in establishing the ages of sediments/ sequence in the studied field.
机译:利用位于尼日尔三角洲沿海和中部沼泽地带的三口井的数据,进行了有孔虫生物地层高分辨率的研究。该研究基于有孔虫指数为中新世尼日尔三角洲早期至中部定义了六个(N6-N15)有孔虫区,这与Blow,1969和Bergreen等,1995相关。有孔虫分析表明,Oshi-13场是钙质和砂质底栖生物,钙质和板状有孔虫非常丰富。化石和索引化石的出现是造成该地区生物地层图和烃饱和度的原因。构造的生物地层图可作为确定研究区域沉积物/层序年龄的基础。

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