首页> 外文期刊>Journal of African Earth Sciences >The biostratigraphic framework of CSDP-003 well, Central Swamp Depobelt, Niger Delta, Nigeria
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The biostratigraphic framework of CSDP-003 well, Central Swamp Depobelt, Niger Delta, Nigeria

机译:尼日利亚尼日尔三角洲中部沼泽Depobelt CSDP-003井的生物地层学框架

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The biostratigraphic framework of CSDP-003 well, Central Swamp Depobelt was investigated to establish the stratigraphic sequences penetrated in the well and the age of the sequences based on calcareous nannofossils recovered. The study was carried out with 138 ditch cuttings from the well and was prepared with the standard simple smear-slide technique of calcareous nannofossil sample preparatory method. The slides produced from the samples were viewed and 31 calcareous nannofossils were recovered which were used to characterize the well into 3 NN zones, following base (Last Downhole Occurrence/First Appearance Datum (LDO/FAD) of Sphenolithus heteromorphus, Top (First Downhole Occurrence/Last Appearance Datum (FDO/LAD) of Helicosphaera ampliaperta, and Top (First Downhole Occurrence/Last Appearance Datum (FDO/LAD) of Sphenolithus heteromorphus corresponding to NN3, NN4, and NN5 biozones respectively. Three Maximum Flooding Surfaces (MFS) and two Sequence Boundaries (SB) were delineated and their ages were determined using the diagnostic forms. MFS 17.40Ma was noted with high abundance and diversity of calcareous nannofossils and explosive events (ACME) of Sphenolithus heteromorphus, Helicosphaera ampliaperta, Sphenolithus moriformis, and Helicosphaera cartari at 2804m within NN4 zone, MFS 15.90Ma was identified based on abundance and diversity peak at 2429m corresponding to explosive events (ACME) of Sphenolithus heteromorphus, and Sphenolithus moriformis within NN4 zone while MFS 15.00Ma was delineated based on abundance and diversity peak with Helicosphaera cartari ACME at 1957m. The Sequence Boundary's SB 16.5 Ma (latest Burdigalian) and SB 15.5 Ma (Langhian) were delineated based on rare to non-occurrence of calcareous nannofossil at 2530m and 2228m respectively.
机译:研究了CSDP-003井(中央沼泽Depobelt)的生物地层学框架,以建立渗透到井中的地层层序,并根据钙质纳米化石回收了该层的年龄。该研究是从井中的138个沟渠切屑中进行的,并使用钙质纳米化石样品制备方法的标准简单涂片滑动技术进行制备。观察了从样品中产生的玻片,并回收了31个钙质纳米化石,将其用于表征该井为3个NN区,之后是Sphenolithus heteromorphus的基础(最后一次井下发生/首​​次出现基准(LDO / FAD)),顶部(第一次下井发生)斜纹螺旋藻的/ Last Appearance Datum(FDO / LAD),以及分别对应于NN3,NN4和NN5生物区的Smorphithus heteromorphus的顶部(首次井下出现/ Last Appearance Datum(FDO / LAD)),三个最大淹水面(MFS)和划定了两个序列边界(SB),并使用诊断形式确定了它们的年龄,注意到MFS 17.40Ma具有高度丰富的钙质纳米化石和多样性,以及异形天竺葵,两面螺旋藻,变形天牛和角叉菜螺的爆炸事件(ACME)。在NN4区2804m处,根据与爆炸e相对应的2429m处的丰度和多样性峰,确定了MFS 15.90Ma在1957m处,利用角叉螺旋藻ACME的丰度和多样性峰勾勒出NN4区域内的Sphenolithus heteromorphus和Moriformis Smorphithus和moriformis的通风孔(ACME)。分别根据2530m和22​​28m钙质纳米化石的稀有到未发生,划定了Sequence Boundary的SB 16.5 Ma(最新的布尔迪加利安)和SB 15.5 Ma(Langhian)。

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