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烧结用焦粉水分及挥发分测量方法的改进 被引量:1
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作者 宾晓燕 《烧结球团》 北大核心 1995年第4期32-37,共6页
烧结用焦粉水分及挥发分测量方法的改进[西班牙]A.Formoso等关键词烧结焦粉,水分,挥发分,测量方法,中子探针,电子探针1前言在烧结厂,为了正确计算烧结混合料中焦炭和铁矿石的配比,迅速得知焦炭和铁矿石水分显得特别... 烧结用焦粉水分及挥发分测量方法的改进[西班牙]A.Formoso等关键词烧结焦粉,水分,挥发分,测量方法,中子探针,电子探针1前言在烧结厂,为了正确计算烧结混合料中焦炭和铁矿石的配比,迅速得知焦炭和铁矿石水分显得特别重要。焦炭是铁矿石烧结的最好燃料,... 展开更多
关键词 烧结焦粉 水分 中子探针 电子探针
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STUDY ON OCCURENCE FORM OF PLATINUM IN XINJIE Cu-Pt DEPOSIT BY NAA AND SCANNING PROTON MICROPROBE 被引量:1
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作者 李晓林 朱节清 +5 位作者 谷英梅 邬显慷 童纯菡 汪云亮 帅德权 张成江 《Nuclear Science and Techniques》 SCIE CAS CSCD 1995年第4期212-216,共5页
A combination of NAA and micro-PIXE was used to study concentrations and distributions of platinum group elements (PGE) in ores from Xinjie Cu-Pt deposit.The NAA results of the bulk indicate that the ores belong to th... A combination of NAA and micro-PIXE was used to study concentrations and distributions of platinum group elements (PGE) in ores from Xinjie Cu-Pt deposit.The NAA results of the bulk indicate that the ores belong to the enriched Pt-Pd type.The element concentration maps of scanning micro-PIXE for the ores show that the occurence form of Pt is independent arsenide minerals. No PGE were detected in chalcopyrite of Xinjie Cu-Pt deposit. These information are economically beneficial to the mineral smelting process. 展开更多
关键词 Platinum group elements Neutron activation analysis Scanning proton microprobe China
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Biogenic characteristics of Mesozoic cherts in southern Tibet and its significance 被引量:1
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作者 何俊国 周永章 李红中 《Journal of Central South University》 SCIE EI CAS 2014年第4期1477-1490,共14页
The Xialu chert, which contains abundant biological information, were investigated by major element analysis, micro-Raman, SEM and EPMA. The results show that SiO2 content of chert is 84.12%-93.08%, averaging 89.84%. ... The Xialu chert, which contains abundant biological information, were investigated by major element analysis, micro-Raman, SEM and EPMA. The results show that SiO2 content of chert is 84.12%-93.08%, averaging 89.84%. The close packed structures of low degree crystallinity of quartz indicate the hydrothermal origin. SiO2 of modern hot springs exhibit loose silica pellets and nodular, beaded structures. Under polarization microscope, the presence of biological skeleton structures indicate that biological activities are involved in the hydrothermal deposition, which correspond to the geochemical characteristics: w(SiO2)/ w(K2O+Na2O), w(SiO2)/w(Al2O3) and w(SiO2)/w(MgO), with average values of 295.29, 68.88 and 284.45, respectively. SiO2 is enriched in the organism(radiolarian) centers, the degree order of SiO2 within the biologic structures is much higher than that of outside. The impurity minerals albites are formed earlier than the original deposition. Kaolinites, feldspars and mixture of organic materials display lower degree of crystallinities and accumulate as vermicular aggregates. 展开更多
关键词 yialu profile chert biological texture hot spring southern Tibet
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