尼日利亚尼日尔三角洲盆地东部沿海沼泽沉积带TTtex-1井孢粉学调查

A. Aturamu
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摘要

对TTtex-1井所穿透地层进行了孢粉相分析,目的是研究TTtex-1井所穿透地层的层序,建立孢粉地层带,确定沉积的相对年龄和古环境。对2179 ~ 3523 m区间内的62个切沟样进行了分析。在样品制备中使用酸进行孢粉相分析。分析结果显示,花粉和孢子的出现量相对较低或较多,小、中、大尺寸孢粉晶ⅰ和孢粉晶ⅱ较多,而ⅲ和孢粉晶ⅳ较少。岩性由页岩和砂岩单元的插层组成,泥质砂岩单元的插层较少,这表明所研究的层段为Agbada组。根据已发现的Multiareolites formosus、Zonocostatites ramonae、Crassoretitriletes vanraadshoveni Verrutricolporites rotundiporus和Racemonocolpites hians等年代指示标志物种,确定了该时期为中新世中期至中新世晚期。提出了2个区间孢粉地层带:formosus - Zonocostatites ramonae, Verrutricolporites rotundiporus - Crassoretitriletes vanraadshoveni。根据孢粉相组合和岩性的古环境解释,所研究的地层层段沉积于海岸-沼泽(边缘海洋)环境。
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Palynological Investigation of TTtex-1 Well, coastal marsh depobelt of Eastern Niger Delta Basin, Nigeria
Palynofacies analyses of the strata penetrated by TTtex-1 Well were carried out with the aim of investigating the stratigraphic sequence penetrated by the Well to establish palynostratigraphic zones, the relative age and the paleoenvironment of deposition. Sixty-two ditch cutting samples within the interval of 2179 – 3523 m were analyzed. The use of acid in the sample preparation for palynofacies analyses were used. The result of the analyses produced relatively low to abundant occurrences of pollen and spores shows abundance of small, medium, and large sizes of palynomacerals I and II, few occurrences of palynomacerals III and IV. The lithology consists of intercalations of shale and sandstone units with few intercalations of argillaceous sandstone units, this designates the studied interval to be Agbada Formation. The interval studied were dated to be middle Miocene to late Miocene based on the recovered age indicative marker species such as Multiareolites formosus, Zonocostatites ramonae, Crassoretitriletes vanraadshoveni Verrutricolporites rotundiporus, and Racemonocolpites hians. A taxon range zone: Ainipollinite verus zone and Two interval range palynostratigraphic zones: Multiareolites formosus – Zonocostatites ramonae, Verrutricolporites rotundiporus - Crassoretitriletes vanraadshoveni were proposed. The stratigraphic interval studied was deposited in the Coastal-marsh (marginal marine) environments based on paleoenvironmental interpretation of the palynofacies associations and the lithology.
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