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五大连池钾质火山岩的Sr、Nd、Pb同位素地球化学及岩浆的化学演化 被引量:20
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作者 王俊文 解广轰 +1 位作者 M.Tatsumoto A.r.basu 《地球化学》 CAS 1988年第4期310-318,共9页
五大连池火山岩是我国东部新生代最典型的钾质玄武岩。以富Ti、Na、K为特点,结晶分异使岩浆向富Si、富碱方向演化。岩石中Rb、Sr、Sm、Nd丰度与熔岩的碱质同步增长。Pb、Sr、Nd同位素组成很特殊,富放射成因Sr和Nd,但贫放射成因Pb,^(87)S... 五大连池火山岩是我国东部新生代最典型的钾质玄武岩。以富Ti、Na、K为特点,结晶分异使岩浆向富Si、富碱方向演化。岩石中Rb、Sr、Sm、Nd丰度与熔岩的碱质同步增长。Pb、Sr、Nd同位素组成很特殊,富放射成因Sr和Nd,但贫放射成因Pb,^(87)Sr/^(86)Sr为0.705100—0.705441,高于全球未分异现代值;^(143)Nd/^(144)Nd为0.512381—0.512433,低于全球未分异现代值;^(206)Pb/^(204)Pb、^(207)Pb/^(204)Pb、^(208)Pb/^(204)Pb分别为16.712—16.992,15.371—15.407,36.515—36.948,比许多大洋玄武岩和大陆玄武岩偏低。上述数据表明,其源区为无明显地壳物质混染的、未遭改造的原始富集地幔,同大洋玄武岩明显不同,暗示地幔的物质组成有区域性和不均匀性。 展开更多
关键词 同位素地球化学 钾质火山岩 岩浆 化学演化
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福建明溪石榴石二辉橄榄岩包体的REE及Pb,Sr,Nd同位素研究 被引量:6
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作者 黄婉康 王俊文 +1 位作者 A.r.basu M.Tatsumoto 《地球化学》 CAS CSCD 北大核心 1992年第2期101-113,共13页
本文研究了明溪地区尖晶石二辉橄榄岩、尖晶石-石榴石二辉橄榄岩和金云母-石榴石二辉橄榄岩包体的REE及Pb,Sr,Nd同位素。它们的Pb,Nd同位素成分表明该区上地幔在67—82km深度上是,MORB型亏损地幔。标本中放射性Sr同位素成分高于“地幔... 本文研究了明溪地区尖晶石二辉橄榄岩、尖晶石-石榴石二辉橄榄岩和金云母-石榴石二辉橄榄岩包体的REE及Pb,Sr,Nd同位素。它们的Pb,Nd同位素成分表明该区上地幔在67—82km深度上是,MORB型亏损地幔。标本中放射性Sr同位素成分高于“地幔系列”可能解释为岛弧区俯冲大洋板块物质的加入。包体的sm-Nd、Rb-Sr年龄可能与十亿年前地幔亏损事件、早古生代H_2O,K_2O等地幔交代作用以及新生代的火山作用过程有关。 展开更多
关键词 石榴石 二辉橄榄岩 包体 同位素
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A rational preparation strategy of phase tuned MoO_(3) nanostructures for high-performance all-solid asymmetric supercapacitor
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作者 M.Kundu D.Mondal +7 位作者 I.Mondal A.Baral P.Halder S.Biswas B.K.Paul N.Bose r.basu S.Das 《Journal of Energy Chemistry》 SCIE EI CSCD 2023年第12期192-206,I0006,共16页
In this work,phase and morphology-tuned MoO_(3) nanostructures are synthesized through a novel modified co-precipitation method,and their electrochemical properties are investigated.For the first time,such a simple su... In this work,phase and morphology-tuned MoO_(3) nanostructures are synthesized through a novel modified co-precipitation method,and their electrochemical properties are investigated.For the first time,such a simple surfactant-assisted synthesis process aided by minor temperature variations is reported which results in phase transition of the nanoparticles from h-MoO_(3) nano-rods to a-MoO_(3) nano-flakes.The nanostructures thus developed are highly porous and crystalline with significantly large specific surface area as compared to previous literature.The theoretical bandgap energy of the optimized sample calculated using Perdew-Zunger local density approximation(LDA) is in good agreement with the experimental findings.An overall structural,morphological,and surface-behavioural analysis predicts the electrochemical superiority in 2D a-MoO_(3).The cyclic voltammetry and galvano-potentiometry measurements of 2D a-MoO_(3) in the potential window of-0.6 V to +0.2 V present the highest pseudosupercapacitive response with a maximum specific capacitance of 829 F g^(-1)at 2 A g^(-1)as compared to h-MoO_(3) (452 F g^(-1)) and h@a-MoO_(3) (783 F g^(-1)).Thus,the MoO_(3) 2D nanostructures synthesized through our novel synthesis technique display excellent specific capacitance as compared to previous reported data.Additionally,a-MoO_(3) exhibits a galvanostatic charging-discharging cyclic stability of about 91%after 2000 cycles,indicating that it can serve as an excellent electrode material for supercapacitors.A solid-state asymmetric supercapacitor device is successfully constructed using a-MoO_(3) which can light up 4 red LEDs for 10 s.The specific energy density of the device reaches a maximum value of 36.3 W h kg^(-1)at the power density of 50 W kg^(-1). 展开更多
关键词 MoO_(3)nanoparticles Asymmetric solid-state supercapacitor Electrochemical performance Low-temperature novel synthesis technique Density functional calculations
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辽宁宽甸黄椅山玄武岩REE及Sr,Nd,Pb同位素组成研究 被引量:3
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作者 解广轰 王俊文 +3 位作者 韦克俭 刘从强 M.Tatsumoto A.r.basu 《中国科学(B辑)》 CSCD 北大核心 1989年第7期752-758,共7页
通过主元素、矿物化学、REE及同位素体系的研究,根据郯庐断裂两侧新生代火山岩的同位素组成有差异的事实,指出由于太平洋板块的俯冲使源区产生壳、幔物质的混合作用和交代作用是导致这种变异的主要原因。交代型超镁铁岩捕虏体含有金云... 通过主元素、矿物化学、REE及同位素体系的研究,根据郯庐断裂两侧新生代火山岩的同位素组成有差异的事实,指出由于太平洋板块的俯冲使源区产生壳、幔物质的混合作用和交代作用是导致这种变异的主要原因。交代型超镁铁岩捕虏体含有金云母和韭闪石,为地幔交代作用提供了实物证据。 展开更多
关键词 玄武岩 REE 同位素 地幔交代作用
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Thermal maturity evaluation using Raman spectroscopy for oil shale samples of USA:comparisons with vitrinite reflectance and pyrolysis methods 被引量:2
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作者 MdGolam Kibria Souvik Das +3 位作者 Qin-Hong Hu Asish r.basu Wen-Xuan Hu Subhadip Mandal 《Petroleum Science》 SCIE CAS CSCD 2020年第3期567-581,共15页
Thermal maturity is commonly assessed by various geochemical screening methods(e.g.,pyrolysis and organic petrology).In this contribution,we attempt to establish an alternative approach to estimating thermal maturity ... Thermal maturity is commonly assessed by various geochemical screening methods(e.g.,pyrolysis and organic petrology).In this contribution,we attempt to establish an alternative approach to estimating thermal maturity with Raman spectroscopy,using 24 North American oil shale samples with thermal maturity data generated by vitrinite reflectance(VRo%)and pyrolysis(Tmax)-based maturity calculation(VRe%).The representative shale samples are from the Haynesville(East Texas),Woodford(West Texas),Eagle Ford and Pearsall(South Texas)Formations,as well as Gothic,Mancos,and Niobrara Formation shales(all from Colorado).The Raman spectra of disordered carbonaceous matter(D1 and G bands separation)of these samples were directly obtained from the rock chips without prior sample preparation.Using the Gaussian and Lorentzian distribution approach,thermal maturities from VR were correlated with carbon G and D1.We found that the Raman band separation(RBS)displayed a better correlation for equivalent VRe%than vitrinite reflectance VRo%.The RBS(D1–G)distance versus total organic carbon,free hydrocarbons from thermal extraction(S1),and the remaining hydrocarbon generating potential(S2)indicate that the RBS(D1–G)distance is also related to kerogen type.Data presented here from three methods of maturity determination of shale demonstrate that Raman spectroscopy is a quick and valid approach to thermal maturity assessment. 展开更多
关键词 US shale Raman spectroscopy Vitrinite reflectance Thermal maturity
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玄武岩中普通辉石、石榴石巨晶的研究(Ⅱ)——Pb、Sr、Nd同位素组成 被引量:2
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作者 王俊文 黄婉康 +2 位作者 解广轰 M.Tatsumoto A.r.basu 《地球化学》 CAS CSCD 北大核心 1992年第1期9-18,共10页
辽宁宽甸、河北汉诺坝及福建明溪碱性玄武岩中普通辉石巨晶的^(87)Sr/^(86)Sr值是0.70387—0.70401,^(143)Nd/^(144)Nd值是0.51282—0.51295,宽甸石榴石巨晶的^(143)Nd/^(144)Nd值是0.51282—0.51293,巨晶的εNd值与载体玄武岩相似。辉... 辽宁宽甸、河北汉诺坝及福建明溪碱性玄武岩中普通辉石巨晶的^(87)Sr/^(86)Sr值是0.70387—0.70401,^(143)Nd/^(144)Nd值是0.51282—0.51295,宽甸石榴石巨晶的^(143)Nd/^(144)Nd值是0.51282—0.51293,巨晶的εNd值与载体玄武岩相似。辉石的^(207)Pb/^(204)Pb值是15.6017—15.6649,^(206)Pb/^(204)Pb值是18.5604—18.8359,石榴石的^(207)Pb/^(204)Pb值是15.6046—15.7792,^(206)Pb/^(204)Pb值是18.1849—19.0345。巨晶放射性Pb同位素明显高于载体玄武岩,表明两者之间未达到同位素平衡。巨晶母岩浆可能产生于二元混合体系,端元之一可能与岛弧物质有关。 展开更多
关键词 玄武岩 辉石 石榴石 巨晶 同位素
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