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Determination of trace elements in high purity nickel by high resolution inductively coupled plasma mass spectrometry 被引量:11
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作者 聂西度 梁逸曾 +1 位作者 唐有根 谢华林 《Journal of Central South University》 SCIE EI CAS 2012年第9期2416-2420,共5页
The contents ofMg, Al, Si, Ti, Cr, Mn, Fe, Co, Cu, Ga, As, Se, Cd, Sb, Pb and Bi in high purity nickel were determined by high resolution inductively coupled plasma mass spectrometry (HR-ICP-MS). The sample was diss... The contents ofMg, Al, Si, Ti, Cr, Mn, Fe, Co, Cu, Ga, As, Se, Cd, Sb, Pb and Bi in high purity nickel were determined by high resolution inductively coupled plasma mass spectrometry (HR-ICP-MS). The sample was dissolved in HNO3 and HCI by microwave digestion. Most of the spectral interferences could be avoided by measuring in the high resolution mode. The matrix effects because of the presence of excess HC1 and nickel were evaluated. Correction for matrix effects was made using Sc, Rh and T1 as internal standards. The optimum conditions for the determination were tested and discussed. The detection limits range from 0.012 to 1.76 ~tg/g depending on the type of elements. The applicability of the proposed method is also validated by the analysis of high purity nickel reference material (NIST SRM 671). The relative standard deviation (RSD) is less than 3.3%. Results for determination of trace elements in high purity nickel were presented. 展开更多
关键词 high resolution inductively coupled plasma mass spectrometry high purity nickel trace element matrix effect internal standard
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Constraints of REE and trace elements of high-pressure-veins and host rocks in western Tianshan on origin of deep fluids in paleosubduction zones 被引量:1
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作者 黄德志 高俊 戴塔根 《Journal of Central South University of Technology》 2005年第2期192-198,共7页
The western Tianshan high-pressure(HP) metamorphic belt represents the paleosubduction mélange of paleozoic south Tianshan ocean between the Yili-central Tianshan and Tarim plates. High-pressure veins are extensi... The western Tianshan high-pressure(HP) metamorphic belt represents the paleosubduction mélange of paleozoic south Tianshan ocean between the Yili-central Tianshan and Tarim plates. High-pressure veins are extensively developed in this HP belt. Compared with normal mid-ocean ridge basalt(N-MORB), the high-pressure veins and host rocks are enriched in light rare earth elements(LREE) and incompatible elements. But high-pressure veins show a larger variation than host rocks in total REE abundance. On the trace element spidergram, all the samples are enriched in incompatible elements and show strong positive Pb anomaly relative to N-MORB. The array tendency lines of plots of the HP rocks have apparent slopes on diagram of m(Sr) vs m(Sr)/m(Zr), m(Li) vs m(Li)/m(Y) and (m(Ce)) vs m(Ce)/m(Pb), which indicates that the enrichment in LREE and incompatible elements relative to N-MORB of the HP-metamorphic rocks from western Tianshan is not attributed to magma evolution process of the protolith. High field strength elements, such as Nb, Ta, Ti, Zr and Hf, do not show negative anomaly relative to N-MORB, which is dissimilar to that of island arc basalts. Therefore, the enrichment in LREE and incompatible elements of the HP rocks is not attributed to the enrichment of the source of the protolith. The mass ratios of Rb to Ba, Ce to Pb, Nb to U and Ta to U of high-pressure veins and host rocks are intermediate of mid-ocean ridge basalt or oceanic island basalt and continental crust. The fluids in western Tianshan paleosubduction zones are mixtures of two sources, dehydration or devolatilization of host rocks and of subducted sediments. 展开更多
关键词 rare earth elements trace element fluid in paleosubduction zone high-pressure vein host rock western Tianshan
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Trace elements spatial distribution characteristics,risk assessment and potential source identification in surface water from Honghu Lake,China
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作者 LIU Chao-yang ZHANG Jing-dong +6 位作者 LI Fei) YANG Jun QIU Zhen-zhen CAI Ying ZHU Li-yun XIAO Min-si WU Zi-xian 《Journal of Central South University》 SCIE EI CAS CSCD 2018年第7期1598-1611,共14页
Five trace elements including Zn, Cu, Cd, Cr and As were investigated in surface water from ten typical sampling sites in Honghu Lake. The consequence indicated that all of the detected trace element levels were withi... Five trace elements including Zn, Cu, Cd, Cr and As were investigated in surface water from ten typical sampling sites in Honghu Lake. The consequence indicated that all of the detected trace element levels were within the allowed standard of China’s safe water guideline. The hazard quotients (HQ) and the hazard index (HI) value levels of all the five heavy metals in all sampling sites did not exceed the acceptable risk limits of non-carcinogenic value through the selected assessment method. Pearson’s correlation analysis and principal component analysis (PCA) indicated that Zn and Cu mainly originated from the natural alluviation and non-point agricultural sources, whereas Cr and As were mainly derived from industrial effluents. Moreover, Cd mainly originated from both non-point agricultural and industrial pollution sources. In addition, cluster analysis (CA) implied that cluster 1 (including S3, S5, S6 and S10) was considered the set of high pollution sites and cluster 2 (including S4 and S9) was identified as the set of moderate pollution sites. 展开更多
关键词 spatial distribution characteristic risk assessment source identification trace elements Honghu Lake
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Effects of Different Compound Trace Element Premixed Materials on Beef Cattle Production Performance and Anti-oxidation Capacity
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作者 Omar Niyaz Omarjan Yakup +3 位作者 Habibulla Ismayil He Zong-lin Saipidin Abla Yao Gang 《Journal of Northeast Agricultural University(English Edition)》 CAS 2019年第4期48-56,共9页
In this study,the effects of two types of premixed materials with different combinations of trace elements on the production performance and antioxidant capacity of simmental beef cattle were examined.Fifteen healthy ... In this study,the effects of two types of premixed materials with different combinations of trace elements on the production performance and antioxidant capacity of simmental beef cattle were examined.Fifteen healthy simmental beef cattle of similar weight(approximately 330 kg),the same age(12 months),without castration,and a good physique were divided into three groups,with five beef cattle in each group.Food of Group Ⅰ beef cattle was supplemented with a commercially marketed 5% compound trace element premixture for fine beef cattle.Food of Group Ⅱ beef cattle was supplemented with a 5% compound microelement premixture for beef cattle that was designed to address local nutrient deficiencies and surpluses.In the blank control group,the beef cattle were not fed a premixture.The pretest period was 15 days,and the test period was divided into prefattening(45 days)and postfattening(45 days)stages.Body weight and body size indices were recorded at 1,2 and 3 months,and blood samples were collected regularly.In Group Ⅰ,the daily weight gain increased significantly by 15.7% compared with that of the control group.The largest daily weight gain was in Group Ⅱ,which increased by 31.6% compared with that in the control.During the test period of 90 days,the body size indices of the three different groups increased in different months,with significant increases in the indices for both test groups compared with those of the control.In Group Ⅰ,the activity of CP,the total activity of SOD and Cu-Zn-SOD increased significantly(p<0.05)compared with those in the control group,with a highly significant increase observed in GSH-PX activity(p<0.01).In Group Ⅱ,the increases in the activity of CP and the total activity of SOD and Cu-Zn-SOD were highly significant compared with those in the control group(p<0.01).In addition,a significant increase was observed in GSH-PX activity(p<0.05).Based on pretest results,the concentrations of Cu,Zn,Mo,Mn,Se and Co in the blood of experimental beef cattle were lower than those of the normal range.After feeding for 90 days,the concentrations of Cu,Zn,Mo,Mn,Se and Co in the blood of Groups Ⅰ and Ⅱ were significantly higher than those in the control group(p<0.05).The concentrations of elements in the blood of Group Ⅱ were close to the appropriate levels.Thus,the effects of the specifically designed compound microelement premixture on the prevention of nutrient imbalances and control of beef cattle nutrition metabolism and the production of fattened beef cattle were significant. 展开更多
关键词 compound trace element premixture simmental beef cattle production performance antioxidant capacity
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Trace Element Geochemistry of the Baishiquan and Pobei Intrusions,Xinjiang,NW China:Petrogenisis Implications
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作者 SONG Xie-Yan,XIE Wei,DENG Yu-Feng(State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China) 《矿物学报》 CAS CSCD 北大核心 2011年第S1期391-391,共1页
The Baishiquan and Pobei Early Permian mafic-ultramafic intrusions were emplaced into Proterozoic metamorphic rocks in the Central Tianshan and the Beishan Fold Belt,northern Xinjiang,NW China.The Baishiquan intrusion... The Baishiquan and Pobei Early Permian mafic-ultramafic intrusions were emplaced into Proterozoic metamorphic rocks in the Central Tianshan and the Beishan Fold Belt,northern Xinjiang,NW China.The Baishiquan intrusion comprises mainly gabbro,and mela-gabbro sills occur within and along the margins of the gabbro body.In the Pobei intrusion,two distinct gabbroic packages,a lower gabbro and the main gabbro,are intruded and overlain by small cumulate wehrlite bodies. 展开更多
关键词 OIB trace element Geochemistry of the Baishiquan and Pobei Intrusions Xinjiang NW China
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Groundwater and Surface Water Contamination of Trace Elements in the Industrial Area of Faisalabad
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作者 Hamaad Raza Ahmad 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期13-13,共1页
An intensive monthly sampling of Madhuana drain at three points and hand pumps from four sites over 12 months covering summer and winter seasons at industrial city of Faisalabad was conducted during August 2000 to Jul... An intensive monthly sampling of Madhuana drain at three points and hand pumps from four sites over 12 months covering summer and winter seasons at industrial city of Faisalabad was conducted during August 2000 to July 2001.Water quality parameters (EC,SAR and RSC) and heavy metal(Cd,Cr,Pb,Ni, Cu,Zn and Mn) pollutants were determined.The results showed that samples collected from Madhuana were found unfit for irrigation owing to high EC,SAR and RSC.Among metal ions the concentration of Cu, Ni,Cr and Mn were found above the safty limits proposed by Ayers and Westcot(1985) while that 展开更多
关键词 surface and GROUNDWATER trace elementS
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Research on Trace Elements Geochemistry of Ordovician Carbonates in Tazhong area,Tarim Basin
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作者 Huajun Wang,Wenhui Huang,Kuangming Zhang,Min Yang School of Energy Resources,China University of Geosciences(Beijing) Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism,Ministry of Education,Beijing 100083,China. 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期145-146,共2页
The research on the trace elements of Ordovician carbonates plays an important role in the whole research work on reservoir in Tazhong area.This work applies ICP-MS,which is a new trace elements analysis technology to... The research on the trace elements of Ordovician carbonates plays an important role in the whole research work on reservoir in Tazhong area.This work applies ICP-MS,which is a new trace elements analysis technology to measure contents of different elements,systematically in the studies of the characteristics and sedimentary settings of Ordovician dolomites in Tazhong area,Tarim Basin,and argues for their enrichment mechanisms and different elements existing pattern.The results show that there is a close relationship between geochemistry charac- 展开更多
关键词 DOLOMITE SEDIMENTARY settings GEOCHEMISTRY trace elements
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Geochemistry of Major and Trace Elements in Natural Waters from the Main Ethiopian Rift:Emphasis on the Source and Occurrence of Fluoride and Arsenic
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作者 Tewodros Rango Gianluca Bianchini +1 位作者 Luigi Beccaluva Renzo Tassinari 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期6-6,共1页
Drinking water supply for the Main Ethiopian Rift (MER) area principally relies on groundwater wells and springs and is characterized by fluoride contamination. New analyses reveal that the F^- geochemical anomaly is ... Drinking water supply for the Main Ethiopian Rift (MER) area principally relies on groundwater wells and springs and is characterized by fluoride contamination. New analyses reveal that the F^- geochemical anomaly is associated with other potentially toxic elements such as As,B,Mo,U,Al,Fe and Mn. Particularly,35%of the 23 investigated groundwater wells and 70%of the 14 hot springs(and 展开更多
关键词 aqueous GEOCHEMISTRY Main ETHIOPIAN RIFT trace elementS TOXIC elementS leaching experiment
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Redistribution of Trace Elements During Shock-inducd Melting and Phase Tranzition of Minerals in the Suizhou l6 Chondrite
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作者 XIE Xiande ZHANG Hong WANG Chunyun 《矿物学报》 CAS CSCD 北大核心 2013年第S1期116-116,共1页
The Suizhou meteorite is an L6 chondrite. This meteorite is consisted of olivine, low-Ca pyroxene, plagioclase, FeNi metal, troilite, whitlockite, chlorapatite, chromite and ilmenite. Olivine and pyroxene grains displ... The Suizhou meteorite is an L6 chondrite. This meteorite is consisted of olivine, low-Ca pyroxene, plagioclase, FeNi metal, troilite, whitlockite, chlorapatite, chromite and ilmenite. Olivine and pyroxene grains display shock-induced mosaic texture, and most plagioclase grains were melted and transformed to maskelynite. This meteorite contains a few very thin shock-produced melt veins ranging from 20 to 100 μm in width. They are chondritic in composition and contain abundant high-pressure minerals in two assemblages. One is the coarse-grained assemblage of ringwoodite, majorite, lingunite with minor amount of tuite, xieite, the CF-phase, akimotoite and amorphized perovskite, and the fine-grained assemblage (the melt vein matrix) composed of majorite-pyrope garnet, magnesiowüstite. FeNi metal and troilite in the Suizhou shock veins were molten and occur as small intergrowth grains or veinlets filling the interstices of garnet crystals or cracks in the vein matrix. It was revealed that olivine, pyroxene and plagioclase in the Suizhou shock veins have transformed in solid state to their high-pressure polymorphs ringwoodite, majorite, and lingunite, respectively, without change in their chemical compositions. 展开更多
关键词 trace element shock MELTING PHASE transition LA-ICP-MS Suizhou METEORITE
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Contents of Trace Metal Elements in Cow Milk Impacted by Different Feedstuffs
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作者 Song Ren-ju Tong Hui-li +1 位作者 Huang Jian-guo Gao Xue-jun 《Journal of Northeast Agricultural University(English Edition)》 CAS 2015年第3期54-61,共8页
Feedstuff intake plays key role in impacting the yield and quality of milk. In this study, we discussed the contents of trace metal elements in cow milk impacted by different feedstuffs. We detected the contents of Pb... Feedstuff intake plays key role in impacting the yield and quality of milk. In this study, we discussed the contents of trace metal elements in cow milk impacted by different feedstuffs. We detected the contents of Pb, Cd, As, Cu, Mg, Ca, Fe and Zn in different feedstuffs and milk by atomic absorption spectrophotometry. The determinations of Pb, Cd and As contents were by graphite furnace A_AS and Cu, Mg, Ca, Fe and Zn was by flame atomic absorption spectrometry. The results showed that Pb, Cd, As and Cu presented in feedstuffs, but Pb, Cd and As were lowly detected in milk samples, and Cu was not detected in milk samples. The content of Mg in concentrates was lower than that in forages. However, the content of Mg in milk from concentrate feed was higher than that in forage feed. This suggested that the utilization of Mg in concentrate feed was higher than that in forage feed. The contents of Ca and Zn were opposite to Mg, and the utilization of Ca and Zn in forage feed was higher than that in concentrate feed. There was no obviously change law of Fe in different feedstuffs and milk samples. The relationship between the contents of trace metal elements in milk to feedstuffs would provide a theoretical basis for dairy farming. It would be useful for improving the milk yield and milk quality of dairy production. 展开更多
关键词 feedstuff cow milk trace metal element CONTENT
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TRACE AND MINOR ELEMENT GEOCHEMISTRY OF XIANGDONG TUNGSTEN DEPOSITS
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作者 Chen Zilong Yang Chuxiong(Department of Geology, Central South University ofTechnology, Changsha 410083, China) 《Journal of Central South University》 SCIE EI CAS 1996年第1期75-77,共3页
Geochemical characteristics of trace and minor elements in some strata of geosynclinal tectonic layer, platform tectonic layer, in granite of Diwa stage, altered rocks and wolframite in the Xiangdong Tungsten Mine are... Geochemical characteristics of trace and minor elements in some strata of geosynclinal tectonic layer, platform tectonic layer, in granite of Diwa stage, altered rocks and wolframite in the Xiangdong Tungsten Mine are systematically studied. Enrichment of W, Sn and Cu in geosynclinal tectonic layer could be one part of mineralization. Different types of alteration might result in variance of distribution of the same trace or minor element. mNb/mTa and mMn/mFe ratios, contents of Nb and Ta in wolframite vary with vein groups′ location. 展开更多
关键词 trace element MINOR element GRANITE tungsten DEPOSITS HUNAN
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北秦岭构造带东段官坡地区花岗伟晶岩锆石U-Pb年代学、岩石成因及其构造背景 被引量:1
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作者 陈国超 张晓飞 +6 位作者 裴先治 李佐臣 李瑞保 王硕 陈孝珍 张荣臻 王永强 《地质学报》 北大核心 2025年第4期1185-1208,共24页
北秦岭构造带花岗伟晶岩是我国重要的伟晶岩矿区,花岗伟晶岩的形成时间和岩石成因存在一定争议。本文通过对北秦岭构造带东段官坡地区峡河村花岗伟晶岩和上河村花岗伟晶岩开展岩石学、锆石U-Pb年代学、锆石Hf同位素地球化学及全岩主微... 北秦岭构造带花岗伟晶岩是我国重要的伟晶岩矿区,花岗伟晶岩的形成时间和岩石成因存在一定争议。本文通过对北秦岭构造带东段官坡地区峡河村花岗伟晶岩和上河村花岗伟晶岩开展岩石学、锆石U-Pb年代学、锆石Hf同位素地球化学及全岩主微量元素地球化学研究,限定北秦岭构造带东段花岗伟晶岩的形成时代,揭示花岗伟晶岩的岩浆来源和岩石成因。LA-ICP-MS锆石U-Pb同位素定年结果显示峡河村花岗伟晶岩和上河村花岗伟晶岩的结晶年龄分别为361~360 Ma和334.8 Ma。峡河村花岗伟晶岩和上河村花岗伟晶岩含有石榴子石、白云母和电气石,富集SiO_(2)、Na_(2)O和K_(2)O,CaO、TFeO和MgO含量较低,主体呈过铝质。峡河村花岗伟晶岩和上河村花岗伟晶岩轻重稀土元素分异不明显,具较明显的Eu正异常;微量元素富集Rb、Th、Ba、Cs等大离子亲石元素(LILE),亏损Nb、Ta、Ti等高场强元素(HFSE),具有低的Nb/Ta和Zr/Hf比值,指示岩浆经历了高度结晶分异作用。峡河村花岗伟晶岩具有较低的ε_(Hf)(t)值,为-11.7~-6.2;上河村花岗伟晶岩ε_(Hf)(t)值明显高于峡河村花岗伟晶岩,为-4.9~1.1。以上结果显示,峡河村花岗伟晶岩为古老地壳部分熔融产物,上河村花岗伟晶岩为新生地壳部分熔融的岩浆在上侵过程中同化混染围岩的结果。北秦岭构造带东段花岗伟晶岩初步可分为北部稀有金属花岗伟晶岩和南部铀花岗伟晶岩。 展开更多
关键词 花岗伟晶岩 微量元素 岩石成因 岩浆演化 北秦岭
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脐血微量元素及氧化/抗氧化因子水平与新生儿呼吸窘迫综合征发病的相关性研究 被引量:1
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作者 黄静 刘晓晨 +3 位作者 高雄 李晓文 李广红 李禄全 《临床儿科杂志》 北大核心 2025年第3期204-210,共7页
目的评估早产儿脐血微量元素及氧化/抗氧化因子水平与新生儿呼吸窘迫综合征(NRDS)发病的相关性,为NRDS的发病机制研究及防治策略提供新思路。方法以2022年12月至2023年12月在新生儿科住院的胎龄<34周早产儿为研究对象。采用火焰原子... 目的评估早产儿脐血微量元素及氧化/抗氧化因子水平与新生儿呼吸窘迫综合征(NRDS)发病的相关性,为NRDS的发病机制研究及防治策略提供新思路。方法以2022年12月至2023年12月在新生儿科住院的胎龄<34周早产儿为研究对象。采用火焰原子吸收法测定微量元素水平,酶联免疫吸附法测定氧化因子丙二醛(MDA)及抗氧化因子超氧化物歧化酶(SOD)水平。比较NRDS组与对照组上述指标的差异,采用受试者工作曲线(ROC)判定各指标预测NRDS发病的价值。结果NRDS组脐血铜水平、锌水平显著低于对照组(P均<0.05)。NRDS组SOD水平低于对照组,MDA水平高于对照组(P均<0.05)。NRDS组SOD/MDA比值显著低于对照组(P<0.001)。脐血锌、铜、SOD、MDA、SOD/MDA预测NRDS发病的AUC分别为0.728、0.917、0.627、0.780、0.824。结论脐血微量元素铜、锌水平降低及氧化/抗氧化因子失衡可能参与早产儿呼吸窘迫综合征发病。 展开更多
关键词 呼吸窘迫综合征 微量元素 超氧化物歧化酶 丙二醛 新生儿
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贵州余庆地区层间破碎带热液型重晶石矿床地球化学特征与成因分析 被引量:1
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作者 李源洪 杜红毅 +3 位作者 陈军 徐石辉 胡涛 袁清松 《地质科技通报》 北大核心 2025年第3期122-133,共12页
热液型重晶石因其高品质而成为近些年的重点勘查对象。位于扬子克拉通中部的武陵-苗岭一带是我国主要的热液重晶石成矿区,已成为重要钡资源基地。近些年,在贵州黔北新发现了受上寒武统娄山关群白云岩与下奥陶统桐梓组底部页岩接触部位... 热液型重晶石因其高品质而成为近些年的重点勘查对象。位于扬子克拉通中部的武陵-苗岭一带是我国主要的热液重晶石成矿区,已成为重要钡资源基地。近些年,在贵州黔北新发现了受上寒武统娄山关群白云岩与下奥陶统桐梓组底部页岩接触部位控制的重晶石矿体,矿体延伸稳定,具有较大的成矿潜力,但其特殊热液成矿机制尚未开展系统研究,制约了进一步的勘查部署工作。以贵州余庆地区热液型重晶石为研究对象,开展了系统的岩相学、主微量元素地球化学和硫同位素组成分析研究。野外地质调查表明,硅(碎屑岩)-钙(白云岩)界面产生的层间破碎带及张性裂隙是该区重晶石的主要控矿构造。元素地球化学分析表明,围岩白云岩样品δCe呈现无异常特征(平均1.06),而重晶石样品呈明显的δCe负异常(平均0.66),揭示重晶石在氧化条件下形成。(Cu+Zn)与Sr元素协变关系和Y/Ho比值指示成矿物质可能来自寒武系富Ba的碳酸盐岩(含膏岩)地层。同样重晶石硫同位素组成(δ34SVCDT为30.94‰~41.27‰)也指示硫主要来自寒武系海相蒸发岩。综合前人研究认为,构造运动驱使盆地流体发生运移,并萃取富Ba蒸发岩地层,在层间断层(硅-钙界面)与大气降水混合,形成重晶石矿床。研究成果为重晶石矿床的勘查提供重要参考。 展开更多
关键词 主微量元素 硫同位素 热液重晶石矿床 余庆地区 贵州 层间破碎带
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四川可尔因矿田锂辉石伟晶岩成因:来自钾长石矿物学、微区地球化学和瑞利分馏模拟的证据 被引量:2
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作者 费光春 谭心 +3 位作者 袁彦伟 陆雪 蔡云华 赵太平 《岩石学报》 北大核心 2025年第6期2161-2178,共18页
可尔因稀有金属矿田位于四川西部,已探明多个花岗伟晶岩型锂辉石矿床,其中李家沟和党坝矿床规模达到了超大型。根据伟晶岩中主要矿物的组成,从可尔因岩体向外,水平方向可分为4个伟晶岩带,依次为微斜长石伟晶岩带(Ⅰ带)、微斜长石钠长石... 可尔因稀有金属矿田位于四川西部,已探明多个花岗伟晶岩型锂辉石矿床,其中李家沟和党坝矿床规模达到了超大型。根据伟晶岩中主要矿物的组成,从可尔因岩体向外,水平方向可分为4个伟晶岩带,依次为微斜长石伟晶岩带(Ⅰ带)、微斜长石钠长石伟晶岩带(Ⅱ带)、钠长石伟晶岩带(Ⅲ带)和钠长石锂辉石伟晶岩带(Ⅳ带)。钾长石是可尔因岩体和不同伟晶岩带中的贯通矿物和造岩矿物,但其组构特征研究较为薄弱,对岩浆演化和稀有金属成矿的指示意义尚不明确。本文以可尔因岩体及各分带伟晶岩中的钾长石为研究对象,对其开展矿物学特征、X射线粉晶衍射、原位微区成分(EPMA和LA-ICP-MS)和瑞利分馏模拟研究。研究结果显示,从可尔因岩体的二云母花岗岩、白云母花岗岩→Ⅰ、Ⅱ、Ⅲ带伟晶岩→Ⅳ带伟晶岩,钾长石中的Li、Rb、Cs等元素含量呈增加趋势,K/Rb比值减小,相较于二云母花岗岩,可尔因矿田的伟晶岩经历了更长的岩浆演化过程。Ⅳ带伟晶岩中钾长石条纹间距明显比Ⅰ-Ⅲ带伟晶岩中钾长石条纹间距小;钾长石的Ti温度计计算结果显示温度降低,表明可尔因伟晶岩演化后期残余熔体具有快速冷却的特征。花岗岩钾长石中P元素含量低于伟晶岩钾长石中P元素含量,指示随岩浆结晶分异,伟晶岩中P元素呈富集趋势。钾长石瑞利分馏模拟显示,从可尔因岩体到伟晶岩存在较好的岩浆演化趋势,指示李家沟和党坝等矿床的锂辉石伟晶岩属于结晶分异成因。 展开更多
关键词 锂辉石伟晶岩 钾长石 微区成分 微量元素模拟 可尔因矿田
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华北克拉通南缘中元古界熊耳群大古石组沉积环境——来自地球化学的证据 被引量:1
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作者 王俊 江武龙 +4 位作者 余雅兰 华仕豪 孔凡浩 袁玉洁 王世炎 《沉积学报》 北大核心 2025年第2期423-438,共16页
【目的】中元古界熊耳群大古石组是华北克拉通南缘变质结晶基底上最早的沉积岩盖层,研究其沉积环境和沉积过程对反演熊耳群早期沉积环境和构造背景,以及哥伦比亚超大陆裂解过程具有重要意义。然而,目前对大古石组仍缺少系统性研究,在沉... 【目的】中元古界熊耳群大古石组是华北克拉通南缘变质结晶基底上最早的沉积岩盖层,研究其沉积环境和沉积过程对反演熊耳群早期沉积环境和构造背景,以及哥伦比亚超大陆裂解过程具有重要意义。然而,目前对大古石组仍缺少系统性研究,在沉积物源和古气候特征方面尤为薄弱。【方法】对豫西北济源小沟背地区熊耳群大古石组进行了主量、微量元素地球化学分析,并探讨了大古石组的物源特征、沉积环境和构造背景。【结果】主量元素分析结果显示,该组细粒碎屑岩离物源区较近,自下而上成分成熟度逐渐降低。其沉积物母岩主要来自长英质岩石和基性岩,自下而上逐渐由花岗岩向长英质火山岩,再到中、基性岩过渡,上段中古老沉积物成分逐渐增加。沉积期间整体为温暖湿润的气候环境,并存在多次气候波动。微量和稀土元素分析结果表明,大古石组下段形成于相对稳定的构造背景,而中、上段形成于较活跃的构造背景。【结论】沉积期间物源、气候及构造环境的变化是地壳活化及与之相关的构造—热作用所致。地幔柱导致地壳上升并逐渐活化,华北克拉通南缘逐渐转入活跃构造背景,大古石组沉积区位于地壳整体抬升的局部凹陷区。熊耳群早期火山活动在局部地区逐渐发育,并给大古石组提供了部分物源。该研究为华北克拉通南缘中元古代早期的构造—沉积演化提供了新证据。 展开更多
关键词 华北克拉通 熊耳群 主量、微量元素 古环境
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安徽铜陵矿集区中生代中酸性侵入岩成因:来自锆石和磷灰石地球化学证据 被引量:1
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作者 徐晓春 余文 +3 位作者 金林森 夏彩莲 谢巧勤 闫峻 《地质学报》 北大核心 2025年第2期480-501,共22页
安徽铜陵矿集区广泛发育中生代中酸性侵入岩,与区内铜金多金属成矿关系密切。关于其成因已有大量研究成果发表,但仍存在争议。本文选择区内铜官山和冬瓜山石英闪长岩以及凤凰山和胡村花岗闪长岩为研究对象,在全岩主微量元素和Sr-Nd同位... 安徽铜陵矿集区广泛发育中生代中酸性侵入岩,与区内铜金多金属成矿关系密切。关于其成因已有大量研究成果发表,但仍存在争议。本文选择区内铜官山和冬瓜山石英闪长岩以及凤凰山和胡村花岗闪长岩为研究对象,在全岩主微量元素和Sr-Nd同位素地球化学研究基础上开展锆石Hf-O同位素以及磷灰石主微量元素地球化学研究,进一步探讨铜陵地区中生代中酸性侵入岩的成因机制。综合前人研究资料和本次工作成果推断,区内中酸性侵入岩主微量元素和稀土元素组成特征基本一致,指示其均属高钾钙碱性岩石系列,具有岛弧型岩浆岩和埃达克岩的特征且富集Sr-Nd同位素。侵入岩体中具有的镁铁质微粒包体以及斜长石反环带结构等岩石学特征,指示这些中酸性侵入岩为壳幔岩浆混合成因。本次工作测得岩石中的锆石ε_(Hf)(t)值介于-20.5~-5.1之间,对应两阶段Hf模式年龄(t_(DM2))为2.9~1.5 Ga,δ^(18)O值介于5.93‰~8.85‰之间,且发现较多年龄分别集中在1.0~0.8 Ga和2.4~2.0 Ga的继承锆石;磷灰石具有高Cl含量(平均值为0.3%)和Cl/F比值、较高REE含量(1714×10^(-6)~5903×10^(-6))及负铕异常(δ(Eu)=0.26~0.68)。基于全岩主微量元素、稀土元素和同位素地球化学特征以及上述锆石和磷灰石地球化学特征,结合区域地质背景和构造演化,本文对前人有关区内中酸性侵入岩不同成因观点进行深入解析,并提出新的成因观点。本研究认为,铜陵矿集区中生代中酸性侵入岩起源于壳幔岩浆混合,即富集岩石圈地幔源岩浆与新元古代新生岛弧地壳源岩浆的混合,上升过程中可能混入了少量古元古代—中元古代古老地壳物质。其中,富集岩石圈地幔源岩浆并非起源于古太平洋俯冲洋壳或俯冲洋壳析出流体交代的上覆岩石圈地幔,而是新元古代华夏洋俯冲析出流体交代扬子板块岩石圈地幔形成的。中生代古太平洋板块俯冲之后的回卷是导致古老造山带加厚再伸展、岩石圈地幔减薄和熔融的地球动力学机制。 展开更多
关键词 锆石U-PB年龄 锆石Hf-O同位素 磷灰石微量元素 中生代中酸性侵入岩 安徽铜陵矿集区
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燕麦籽粒四种矿质元素含量与其在土壤中有效态含量的相关性分析 被引量:1
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作者 祝天天 贺鹏 +2 位作者 李军辉 安桦 杨珍平 《麦类作物学报》 北大核心 2025年第4期502-509,共8页
为探究Zn(锌)、Fe(铁)、Ca(钙)、B(硼)4种矿质元素在燕麦籽粒中的含量与其在土壤中的有效态含量的相关性,在山西省燕麦种植面积较大的3个区县(朔州市平鲁区、右玉县和大同市左云县),选取了240个村庄的332个点位,采集耕层土壤,并收集其... 为探究Zn(锌)、Fe(铁)、Ca(钙)、B(硼)4种矿质元素在燕麦籽粒中的含量与其在土壤中的有效态含量的相关性,在山西省燕麦种植面积较大的3个区县(朔州市平鲁区、右玉县和大同市左云县),选取了240个村庄的332个点位,采集耕层土壤,并收集其上种植收获的燕麦籽粒样品,检测4种元素在土壤中的有效态含量和在燕麦籽粒中的含量,并分析二者的相关性。结果表明:(1)4种元素在3个生产区土壤中的有效态含量表现为Ca>Fe>Zn>B,且Ca含量属于高水平,Fe、Zn、B含量属于中等或低水平;在同一区县不同采样点间,土壤有效Zn含量差异较大,有效Ca含量差异较小,另两种元素含量的差异性介于二者之间。(2)4种元素在燕麦籽粒中的平均积累量为Ca>Fe>B>Zn,与其他学者的研究结果相比,Fe与Zn的平均含量相对较低,Ca的平均含量相对较高;同一区县不同采样点间,燕麦籽粒中B积累量差异较大,Zn积累量差异较小,Fe、Ca积累量差异居中。(3)经相关分析,土壤中有效态Zn、Fe、B含量间存在显著正相关关系(P<0.05),三种元素含量与Ca含量的相关程度存在地区差异;燕麦籽粒中Zn、Fe、B含量与Ca的积累量呈正相关;4种元素在燕麦籽粒中的积累量与其在土壤中的有效态含量的相关性在三个县区表现不一,其中在土壤有效态含量尤其Ca含量相对较高的右玉县,燕麦籽粒Zn含量与土壤有效态Zn、Ca、B含量均呈显著正相关。综上,本试验所在燕麦生产区,土壤有效态Fe、Zn、B含量与燕麦籽粒中Fe、Zn、B含量均有提升空间;钙质土壤区适当降低土壤有效态Ca含量有助于促进燕麦籽粒Ca积累。 展开更多
关键词 燕麦 中微量元素 有效态含量 籽粒矿质元素 相关性分析
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粤北下庄花岗岩体岩石成因与铀成矿关系:锆石微量元素和矿物化学的约束 被引量:2
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作者 陶继华 张泽凤 +7 位作者 任志 徐志添 孙俊杰 曹俊 苏献源 冷成彪 许德如 杨跃贵 《地质学报》 北大核心 2025年第5期1656-1675,共20页
华南花岗岩型铀矿床常常与U含量大于10×10^(-6)的富U花岗岩在空间上紧密相关,了解这些富U产铀花岗岩的岩石成因有助于铀矿找矿勘探和铀成矿理论研究。本文以下庄富U花岗岩为研究对象,开展系统的锆石U-Pb年代学和锆石微量元素特征,... 华南花岗岩型铀矿床常常与U含量大于10×10^(-6)的富U花岗岩在空间上紧密相关,了解这些富U产铀花岗岩的岩石成因有助于铀矿找矿勘探和铀成矿理论研究。本文以下庄富U花岗岩为研究对象,开展系统的锆石U-Pb年代学和锆石微量元素特征,以及黑云母和绿泥石矿物地球化学成分研究。结果显示,下庄花岗岩形成年龄为236~234 Ma。下庄花岗岩来自古元古代沉积岩部分熔融,熔体具有高F含量特征,经历了较高程度的分离结晶作用,随着岩浆演化,氧逸度逐渐降低,U元素不断富集,最终形成了含大量晶质铀矿、独居石、磷钇矿和钍石等富U副矿物的富U(>10×10^(-6))花岗岩。由于受到燕山期基性岩浆作用形成的相对酸性和低氧化性热液流体影响,下庄花岗岩中富U副矿物中的U元素被大量萃取,成为铀矿化作用的重要成矿物质来源。 展开更多
关键词 富U花岗岩 花岗岩型铀矿床 锆石微量元素 矿物地球化学 下庄花岗岩
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锌肥随水滴施对新疆绿洲棉田土壤养分的影响
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作者 李全胜 高志建 +2 位作者 于航 王国栋 刘瑜 《新疆农业科学》 北大核心 2025年第6期1308-1317,共10页
【目的】研究随水滴施锌肥对棉田土壤养分的影响,为指导锌肥随水滴灌施用提供理论依据。【方法】设置田间小区试验,在棉花生育期设置随水滴施不同用量锌肥处理,分别为0 kg/hm^(2)(CK)、7.5 kg/hm^(2)(Zn1)、15 kg/hm^(2)(Zn2)、22.5 kg/... 【目的】研究随水滴施锌肥对棉田土壤养分的影响,为指导锌肥随水滴灌施用提供理论依据。【方法】设置田间小区试验,在棉花生育期设置随水滴施不同用量锌肥处理,分别为0 kg/hm^(2)(CK)、7.5 kg/hm^(2)(Zn1)、15 kg/hm^(2)(Zn2)、22.5 kg/hm^(2)(Zn3)、30 kg/hm^(2)(Zn4)、37.5 kg/hm^(2)(Zn5)、45 kg/hm^(2)(Zn6),分析不同锌肥滴施用量条件0~20 cm和20~40 cm土壤中主要养分含量的变化特征。【结果】随着锌肥施用量的增加,0~20 cm土层有效锌含量呈逐渐增加趋势,20~40 cm土层呈波动变化;同不施锌肥相比,锌肥施用降低了0~20 cm和20~40 cm棉田土壤pH值,并提高碱解氮、有效磷含量,其中碱解氮、有效磷含量均在Zn3处理时含量最高,分别为84.16和84.68 g/kg、31.93和30.40 g/kg;0~20 cm和20~40 cm棉田土壤速效钾、有效铁含量随着锌肥施用量的增加呈先增加后降低的趋势,并且均在Zn4处理时含量最高,为548.33和552.00 g/kg、10.35和10.55 mg/kg;0~20 cm和20~40 cm棉田土壤有效锰和交换性镁随着锌肥施用量的增加呈逐渐增加的趋势,并且均在Zn6处理时含量最高,分别为5.0和5.0 mg/kg、4.48和4.48 mg/kg。【结论】不同锌肥用量试验,当硫酸锌滴施量为22.5~30.0 kg/hm^(2)时,土壤pH值下降,碱解氮、有效磷、速效钾、有效锌、有效铁含量均处于较高值,有效锰、交换性镁则在锌滴施量为45 kg/hm^(2)时,含量最高,滴施锌肥对提升新疆绿洲棉田灌耕灰漠土的土壤肥力有正向的作用。 展开更多
关键词 锌肥 随水滴施 棉花 土壤养分 微量元素
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