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1.
Magneticmineralsintheloess paleosolseriesaccountforabout 1 % -2 %ofthetotal (LiuTungshengandZhangZhonghu ,1 962 ) .Duetotheiraerolianorigin ,themagneticmineralsarecomplicatedincomposition ,largeingrainsizerange ,andsignificantlydifferentincrystallinity .Asaresult,researchonthesemagneticmineralswouldbesetwithalotofdifficulties.Previousre searchersemployedopticalmicroscopic ,X raydiffractionandM ssbauerspectrometrictechniquestostudythemagneticmineralsintheloess paleosolseries,andchieflyontheb… 相似文献
2.
从西峰和段家坡黄土剖面S5-1层段中分选出<30μm粒级、磁性相对最强的组分(分别为XS-4J和DS-4J),先后进行了MPV-3光学显微镜的观察与反射率测定、矿物的扫描电镜能谱测定和X射线衍射物相分析.两个样品的磁性矿物均以风尘碎屑状的钛铁氧化物为主.XS-4J样矿物的反射率和Fe的含量都普遍较高,磁性矿物除磁(赤)铁矿、赤铁矿外还见有含铁高的氧化物(Fe 72.20%~86.70%,质量分数)和含Cr、Ni的钛铁晶石或钛铁矿.DS-4J样的磁性矿物中Fe与Ti元素呈明显的负线性相关关系,Si、Al、Ca的含量较高,矿物以磁(赤)铁矿、赤铁矿、针铁矿和褐铁矿为主,并明显见有磁性矿物被溶蚀和新生的磁(赤)铁矿.磁性矿物成分与组合特征的差异反映了西峰与段家坡S5-1岩石中磁性矿物的物质来源与保存条件有较明显的差异. 相似文献
3.
Aierken Sidike Alifu Sawuti Xiang-Ming Wang Heng-Jiang Zhu S. Kobayashi I. Kusachi N. Yamashita 《Physics and Chemistry of Minerals》2007,34(7):477-484
The photoluminescence and excitation spectra of sodalites from Greenland, Canada and Xinjiang (China) are observed at 300
and 10 K in detail. The features of the emission and excitation spectra of the orange-yellow fluorescence of these sodalites
are independent of the locality. The emission spectra at 300 and 10 K consist of a broad band with a series of peaks and a
maximum peak at 648 and 645.9 nm, respectively. The excitation spectra obtained by monitoring the orange-yellow fluorescence
at 300 and 10 K consist of a main band with a peak at 392 nm. The luminescence efficiency of the heat-treated sodalite from
Xinjiang is about seven times as high as that of untreated natural sodalite. The emission spectrum of the S2
− center in sodalite at 10 K consists of a band with a clearly resolved structure with a series of maxima spaced about 560 cm−1 (20–25 nm) apart. Each narrow band at 10 K shows a fine structure consisting of a small peak due to the stretching vibration
of the isotopic species of 32S34S−, a main peak due to that of the isotopic species of 32S2
− and five peaks due to phonon sidebands of the main peak. 相似文献