General geology and geochemistry of the Lokpanta Formation oil shale, Nigeria

IF 1.3 4区 工程技术 Q4 ENERGY & FUELS
Oil Shale Pub Date : 2021-01-01 DOI:10.3176/OIL.2021.1.01
S. Ofili, A. Soesoo
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引用次数: 8

Abstract

. A detailed geochemical and mineralogical study was carried out on the Lokpanta oil shale (OS), Nigeria. Samples from three drill cores and several outcrops were studied in order to understand OS general geochemistry and reconstruct tectonic and depositional settings as well as paleoredox conditions. The mineral phases in OS include calcite, quartz, dolomite, feldspar, illite, kaolinite, halloysite, pyrite and gypsum, as well as a trace amount of anatase. The Lokpanta oil shale shows little variation in geochemistry. It is depleted in trace elements Ba and Rb and major compounds except CaO, and is enriched in trace elements Mo, Sb, As, V, Zn, Ni and U with reference to the Post-Archean Australian Shale (PAAS). These enrichments are, however, in most cases lower than those in the Estonian graptolite argillite (GA). Trace element ratios (U/Th, Ni/Co, V/Ni, V/(V + Ni) V/(V + Cr)) indicate that the Lokpanta oil shale was deposited in an anoxic environment. Discriminant diagrams also suggest its deposition in an active continental margin setting and a transitional to marine environment. The geochemical and paleoenvironmental features of the Lokpanta oil shale were compared with those of the Estonian graptolite argillite .
尼日利亚Lokpanta组油页岩一般地质地球化学特征
。对尼日利亚Lokpanta油页岩(OS)进行了详细的地球化学和矿物学研究。研究了三个岩心和几个露头样品,以了解OS的一般地球化学特征,重建构造和沉积环境以及古氧化还原条件。OS中的矿物相包括方解石、石英、白云石、长石、伊利石、高岭石、高岭石、黄铁矿和石膏,以及微量锐钛矿。Lokpanta油页岩地球化学特征变化不大。后太古宙澳大利亚页岩(PAAS)中微量元素Ba、Rb及除CaO外的主要化合物均富集,微量元素Mo、Sb、As、V、Zn、Ni、U富集。然而,在大多数情况下,这些富集程度低于爱沙尼亚笔石泥质岩的富集程度。微量元素比值(U/Th、Ni/Co、V/Ni、V/(V + Ni) V/(V + Cr))表明Lokpanta油页岩沉积于缺氧环境。判别图还表明其沉积于活动大陆边缘环境,并向海洋环境过渡。对比了Lokpanta油页岩与爱沙尼亚笔石泥岩的地球化学和古环境特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Oil Shale
Oil Shale 工程技术-工程:石油
CiteScore
2.90
自引率
15.80%
发文量
14
审稿时长
4.2 months
期刊介绍: The Oil Shale is a scientific-technical open access journal published by the Estonian Academy Publishers in collaboration with the University of Tartu, Tallinn University of Technology, and the Estonian University of Life Sciences.
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