搜索结果: 1-2 共查到“地质学 Mm”相关记录2条 . 查询时间(0.406 秒)
风成沉积物4~16 mm石英氧同位素记录及其物质来源意义
石英氧同位素比值 大气粉尘 物质来源
2009/3/19
通过对灵台剖面7.0 MaBP以来的黄土-红粘土堆积以及黄土高原和北京6个马兰黄土剖面的石英氧同位素分析, 发现石英氧同位素比值受沉积后作用的影响不明显, 同一粒径颗粒的石英氧同位素比值比较能够较好地反映源区变化特征; 灵台剖面红粘土的氧同位素比值的变化范围以及波动特征和第四纪黄土-古土壤相似, 表明红粘土和其上的黄土有类似的沉积物源系统; 此外, 整个剖面上的石英氧同位素比值的波动可能仅反映了物...
Third-generation synchrotron x-ray diffraction of 6-mm crystal of raite, 'Na3Mn3Ti0.25Si8O20(OH)2z10H2O, opens up new chemistry and physics of low-temperature minerals
Third-generation synchrotron x-ray diffraction low-temperature minerals chemistry and physics
2011/11/11
The crystal structure of raite was solved and refined from data collected at Beamline Insertion Device 13 at the European Synchrotron Radiation Facility, using a 3 3 3 3 65 mm single crystal. The refi...