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Trace and rare earth element geochemistry of the black and grey shales of the Calabar Flank, Southeastern Nigeria: constraints on the depositional environment and the degree of metal enrichment 被引量:1
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作者 Christopher Iorfa Adamu Benjamin Odey Omang +2 位作者 Oluwaseye Peter Oyetade Otu Johnson Therese Ntonzi Nganje 《Acta Geochimica》 EI CAS CSCD 2021年第3期312-324,共13页
This study focuses on the trace and rare earth elements(REE)geochemistry of the Nkporo and Ekenkpon Shales of the Calabar Flank.The main aim is to infer their depositional environment and the degree of their metal enr... This study focuses on the trace and rare earth elements(REE)geochemistry of the Nkporo and Ekenkpon Shales of the Calabar Flank.The main aim is to infer their depositional environment and the degree of their metal enrichment.The shale samples were analyzed using inductively coupled plasma mass spectrometry.The results indicated that the mean concentrations of K,Na,and Fe in Nkporo and Ekenkpon Shales are 1.45,0.4,and 4.17 wt%,and 1.11,0.44,and 5.42 wt%;respectively.The Nkporo Shale is enriched with the following trace elements;P>Mn>Sr>Ba>Zn>Ce>Rb>Zr>V>Cr>Ni and depleted in the following trace elements;Ta>Ge>Sb>Bi>Cd>Ag>Te>In>Hg.While the Ekenkpon Shale is enriched with the following trace elements;P>Mn>Ba>Sr>V>Ce>Zr>Rb>Cr>Zn>Ni and depleted in;Sb>Ge>Bi>Ag>Ce>Te>In>Hg.The concentration of redox-sensitive elements such as V,Ni,Mo,U,Cu,Cr,Re,Cd,Sb,Ti,Mn,and their ratio V/Mo and U/Mo in the black and grey shale samples show different patterns.The REE obtained from the Nkporo and Ekenkpon Shales were PAAS normalized.The Nkporo Shale showed a slightly flat light rare-earth element(LREE),middle rare-earth element(MREE),and heavy rare earth element(HREE)pattern enrichment.Ce/Ce*ranges from 0.95 to 1.09 in Nkporo Shale and 0.67 to 1.40 in Ekenkpon Shale.The Ekenkpon Shale showed a slight LREE,MREE enrichment,and depleted HREE patterns.The Mn contents and U/Mo ratio in Nkporo and Ekenkpon Shales suggests a poor oxygen transitional environment.The V/Mo and V/(V+Ni)ratios indicated that the Nkporo shales were deposited in an anoxic to suboxic conditions and Ekenkpon shales were also deposited under an anoxic to suboxic conditions.The V/Ni ratio indicated that the organic matter in the Nkporo shale is terrigenous while that of the Ekenkpon shales are both terrigenous and marine in origin. 展开更多
关键词 rare-earth elements(ree) Trace elements Calabar Flank SUBOXIC ANOXIC
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南秦岭地区下寒武统黑色页岩赋存的千家坪大型钒矿地球化学特征及成矿环境 被引量:12
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作者 徐林刚 付雪瑞 +3 位作者 叶会寿 郑伟 陈勃 方正龙 《地学前缘》 EI CAS CSCD 北大核心 2022年第1期160-175,共16页
南秦岭地区下寒武统黑色页岩是我国主要的富钒层位,其中千家坪大型钒矿是典型代表。矿体主要赋存在水沟口组第一岩性段的碳硅质岩石中。为了探讨钒矿的成矿物质来源和南秦岭早寒武世古海洋氧化-还原环境,本文对水沟口组第一岩性段富钒... 南秦岭地区下寒武统黑色页岩是我国主要的富钒层位,其中千家坪大型钒矿是典型代表。矿体主要赋存在水沟口组第一岩性段的碳硅质岩石中。为了探讨钒矿的成矿物质来源和南秦岭早寒武世古海洋氧化-还原环境,本文对水沟口组第一岩性段富钒碳硅质岩和上覆的第二岩性段泥质灰岩开展了岩石地球化学研究。第一岩性段碳硅质岩比第二岩性段泥质灰岩具有更高的Y/Ho比值,说明碳硅质岩主要为海水自生沉积形成的,而泥质灰岩的物质组成主要来自陆源碎屑。Eu/Eu^(*)与V含量不具备正相关关系,且Y/P_(2)O_(5)-Zr/Cr和Fe/Ti-Al/(Al+Fe+Mn)图解均显示钒矿主要是海水沉积形成的,热液作用对成矿元素的富集贡献很小。水沟口组样品Ce/Ce^(*)均为负异常,变化范围为0.26~0.96,第一岩性段钒矿石比第二岩性段泥质灰岩具有高Mo/Sc、V/Sc、V/Cr比值,低Th/U比值的特征,反映了早寒武世早期南秦岭为氧化-还原分层的古海洋结构,而晚期古海洋则全部被氧化。 展开更多
关键词 千家坪钒矿 微量元素 稀土元素 矿床成因 氧化-还原环境 南秦岭
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湘西北叶溪育含钒石煤矿地质特征及稀土元素分析 被引量:3
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作者 江新华 《中国煤炭地质》 2010年第B08期4-7,共4页
叶溪育石煤是湖南省境内一种比较特殊的煤种,其赋矿层位属"下寒武统黑色含矿岩系",主要分布于寒武系下统小烟溪组下段,一般含石煤层3层,个别地段为4-5层。叶溪育石煤矿可采石煤主要为第二层,厚度4.98~9.18m,平均7.49m。该矿... 叶溪育石煤是湖南省境内一种比较特殊的煤种,其赋矿层位属"下寒武统黑色含矿岩系",主要分布于寒武系下统小烟溪组下段,一般含石煤层3层,个别地段为4-5层。叶溪育石煤矿可采石煤主要为第二层,厚度4.98~9.18m,平均7.49m。该矿石煤分布面积大,层位稳定,连续性较好;原煤发热量3.52~10.23MJ/kg,灰分产率52.12%~74.32%,全硫平均含量1.56%,为中硫、高灰分、低发热量的劣质煤;煤系地层中同时含钒矿体Z1、Z2、Z3,呈似层状、透镜状产出,其中Z1矿体已达中型规模;根据稀土元素地球化学分析,含煤岩系形成于缺氧的还原环境,矿床成因属于生物地球化学沉积矿床。 展开更多
关键词 含钒石煤 矿床地质特征 煤质特征 稀土元素 湘西北叶溪育
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The Influence of <i>γ</i>-Irradiation on Thermoemf and Heat Conduction of Ln<sub>0.01</sub>Sn<sub>0.99</sub>Se (Ln - Pr, Tb, Er) Monocrystals
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作者 Jahangir Islam Huseynov Tapdiq Aslan Jafarov 《World Journal of Condensed Matter Physics》 2014年第1期1-5,共5页
Monocrystals are synthesized and grown according to Bridgman-Stockbarger method, and the influence of rare earth elements (REE) as well as of γ-irradiation on electrophysical properties of (SnSe)1-x - (SnSe)x (Ln - P... Monocrystals are synthesized and grown according to Bridgman-Stockbarger method, and the influence of rare earth elements (REE) as well as of γ-irradiation on electrophysical properties of (SnSe)1-x - (SnSe)x (Ln - Pr, Tb, Er) alloy system is investigated. During transition from SnSe to (SnSe)1-x - (SnSe)x solid solutions, a partial compensation of charge carriers occurs and additional scattering centres appear. At low temperatures T after irradiation with γ-quanta, thermoemf in samples of p-type conduction becomes higher and decreases in those of n-type conduction. In addition, under the influence of γ-rays radiation, defects come into being causing a decrease in lattice heat conduction and a rise in electron heat conduction. REE impurities are supposed to be positioned among the points of crystal lattice during irradiation with γ-quanta and, moreover, Frenkel defects are formed. 展开更多
关键词 Thermoemf Heat Conduction rare-earth elements (ree) Thermal Resistance Γ-IRRADIATION Radiation-Induced Defects
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Global glance
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《China Rare Earth Information》 2017年第4期6-8,共3页
Queensland could likely play host to a number of rare minerals, as geologists have unearthed evidence suggesting the presence of platinum and gold, as well as rare-earth elements (REE). "This may be a whole new f... Queensland could likely play host to a number of rare minerals, as geologists have unearthed evidence suggesting the presence of platinum and gold, as well as rare-earth elements (REE). "This may be a whole new frontier for Queensland," Natural Resources and Mines Minister Dr Anthony Lynham said over the weekend. "Beyond the potential economic boost for Queensland, the discovery brings a new understanding of mineral potential in a previously under-explored area." 展开更多
关键词 Queensland could LIKELY play host to a number of rare minerals AS geologists have unearthed evidence suggesting the PRESENCE of platinum and gold AS well AS rare-earth elements (ree).
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Controls of interactions between iron hydroxide colloid and water on REE fractionations in surface waters:Experimental study on pH-controlling mechanism 被引量:2
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作者 刘丛强 吴佳红 于文辉 《Science China Earth Sciences》 SCIE EI CAS 2002年第5期449-458,共10页
The influence of pH on the partitioning behavior of REE at the water/particulate interface has been studied experimentally. At the beginning of colloid formation the adsorption of REE on iron hydroxide colloids is dom... The influence of pH on the partitioning behavior of REE at the water/particulate interface has been studied experimentally. At the beginning of colloid formation the adsorption of REE on iron hydroxide colloids is dominant, followed by REE desorption. Finally adsorption and desorption tend to reach equilibration. The capability of iron hydroxide colloids to adsorb the HREE is greater than that to adsorb the LREE. With increasing pH, LREE/HREE fractionations will take place between iron hydroxide colloids and water, leading to the reduction of their partition coefficient ratio (DLREE/DHREE). The DREE distribution patterns show Y anomalies (DY/DHo <1), with obvious REE tetrad effects appearing under low pH conditions. Experimental results have shown that there do exist REE tetrad effects in nature. In addition to pH, the chemical type of surface water and ion intensity are also the important factors controlling REE tetrad effects and leading to fractionations between particulate-adsorbed REE and dissolved REE. 展开更多
关键词 rare-earth elements (ree) adsorption TETRAD effect interaction at the water/particulate interface.
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Separation and recovery of critical metal ions using ionic liquids 被引量:1
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作者 Terence Makanyire Sergio Sanchez-Segado Animesh Jha 《Advances in Manufacturing》 SCIE CAS CSCD 2016年第1期33-46,共14页
Separation and purification of critical metal ions such as rare-earth elements (REEs), scandium and niobium from their minerals is difficult and often deter- mines if extraction is economically and environmentally f... Separation and purification of critical metal ions such as rare-earth elements (REEs), scandium and niobium from their minerals is difficult and often deter- mines if extraction is economically and environmentally feasible. Solvent extraction is a commonly used metal-ion separation process, usually favored because of its sim- plicity, speed and wide scope, which is why it is often employed for separating trace metals from their minerals. However, the types of solvents widely used for the recovery of metal ions have adverse environmental impact. Alternatives to solvent extraction have been explored and advances in separation technologies have shown commer- cial establishment of liquid membranes as an alternative to conventional solvent extraction for the recovery of metals and other valuable materials. Liquid membrane transport incorporates solvent extraction and membrane separation in one continuously operating system. Both methods con- ventionally use solvents that are harmful to the environ- ment, however, the introduction of ionic liquids (ILs) over the last decade is set to minimize the environmental impact of both solvent extraction and liquid membrane separation processes. ILs are a family of organic molten salts with low or negligible vapour pressure which may be formed below 100 ~C. Such liquids are also highly thermally stable and less toxic. Their ionic structure makes them thermody- namically favorable solvents for the extraction of metallic ions. The main aim of this article is to review the current achievements in the separation of REE, scandium, niobium and vanadium from their minerals, using ILs in eithersolvent extraction or liquid membrane processes. The mechanism of separation using ILs is discussed and the engineering constraints to their application are identified. 展开更多
关键词 Critical metals Ionic liquids (ILs) -Niobium Tantalum rare-earth elements (rees)vanadium SCANDIUM
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