尼日利亚东南部Calabar翼白垩系页岩矿物学和理化性质:古风化条件、物源和工业应用意义

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Solid Earth Sciences Pub Date : 2022-06-15 DOI:10.1016/j.sesci.2021.10.001
Christopher I. Adamu, Oluwaseye P. Oyetade, Azubuike S. Ekwere, Ebenezer A. Kudamnya, Kehinde I. Adebayo, Idara A. Uyok, Therese N. Nganje
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引用次数: 2

摘要

对尼日利亚东南部Calabar翼白垩系页岩的物化、矿物学性质、古风化条件和工业应用进行了研究。利用x射线荧光、x射线衍射(XRD)、扫描电子显微镜(SEM)和岩土工程技术对Ekekpon和Nkporo地层的20个页岩样品进行了分析。主要元素氧化物分析结果表明,恩波罗页岩富含SiO2;氧化铝的在量比;Fe2O3祝辞而Ekepkon页岩也富含SiO2;氧化铝的在量比;Fe2O3祝辞曹比;K2O。XRD分析表明,高岭石是主要的粘土矿物,其他非粘土矿物有石英、缬长石、云母、橄榄石、钠云石等。扫描电镜显示,鄂克普孔页岩富钙。对比矩阵显示,SiO2主要存在于恩波罗页岩的石英相中,而在埃克孔页岩中SiO2主要存在于粘土相中。元素比值和判别图显示,页岩物源为中基性火成岩,构造背景为陆洋弧。恩波罗页岩中存在高岭石,蚀变化学指数(CIA)值在83.58 ~ 96.93之间,表明该页岩来源于源区强烈的化学风化作用。鄂肯坡页岩的CIA值较低(37.90 ~ 76.96),主要是由于页岩中CaO和钙富集,且页岩中石英和高岭石含量高,推测其形成于烃源区中度至强烈的风化作用。土工性能表明,两种页岩都适合用于陶瓷和耐火材料工业。埃肯蓬页岩适合作为填充材料和水泥工业的原材料。然而,由于氧化铁、石灰、氧化镁、碳酸钾和苏打含量高,这些页岩不符合造纸和橡胶生产的规格。
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Mineralogical and physico-chemical properties of the Cretaceous shales of the Calabar Flank, south-eastern, Nigeria: Implication for paleo-weathering conditions, provenance and industrial applications

The Physico-chemical and mineralogical properties of the Cretaceous shales of Calabar Flank southeastern Nigeria were examined for their Provenance, Paleo-weathering Conditions and Industrial Applications. Twenty samples of shale from Ekekpon and Nkporo Formations were analysed using X-Ray Fluorescence, X-ray diffraction (XRD), scanning electron microscopy (SEM) and geotechnical techniques. Results from the major oxides of elements revealed that the Nkporo Shale is enriched with SiO2 > Al2O3 > LOI > Fe2O3 > SO3 while the Ekepkon shale is also enriched in SiO2 > Al2O3 > LOI > Fe2O3 > CaO > K2O. The XRD revealed kaolinite as the major clay mineral, while other non-clay minerals are quartz, vallerite, mica, nacaphite, sodalite. The SEM shows that the Ekepkon Shale is enriched in calcium. The correlation matrix revealed SiO2 resides more in the quartz phase of the Nkporo Shales, while in the Ekekpon Shale the SiO2 is associated with the clay. The element ratios and discrimination diagrams revealed that the provenance of the shales is of intermediate to mafic igneous rocks and a tectonic setting of continental to oceanic arcs. The presence of kaolinite in the Nkporo Shale with the chemical index of alteration (CIA) values ranging from 83.58 to 96.93, indicated that the shale is derived from intensive chemical weathering in the source area. The low CIA values (37.90–76.96) in Ekenkpon Shale is attributed to CaO and calcium enrichment in the shale and the shale contains high quartz and kaolinite therefore the shale is suggested to have been derived from an intermediate to intense weathering activities in the source area. The geotechnical properties revealed that both shales are suitable for ceramic and refractory industries. The Ekenkpon Shale will be suitable for use as filling material and as raw material in cement industries. However, the shales do not meet the specifications for paper and rubber production due to the high contents of iron oxide, lime, magnesia, potash and soda.

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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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