期刊文献+
共找到2篇文章
< 1 >
每页显示 20 50 100
天然和实验冲击球粒陨石矿物的变形变质比较研究
1
作者 谢先德 陈鸣 +1 位作者 戴诚达 a.el.goresy 《矿物岩石地球化学通报》 CAS CSCD 1997年第S1期5-7,共3页
天然和实验冲击球粒陨石矿物的变形变质比较研究谢先德陈鸣戴诚达(中国科学院广州地球化学研究所,广州510640)A.El.Goresy(Max-PlanckInstitutfurKernphysik,69029Heid... 天然和实验冲击球粒陨石矿物的变形变质比较研究谢先德陈鸣戴诚达(中国科学院广州地球化学研究所,广州510640)A.El.Goresy(Max-PlanckInstitutfurKernphysik,69029Heidelberg,Germany)关键... 展开更多
关键词 冲击 球粒陨石 矿物变形变质
在线阅读 下载PDF
THE CHEMICAL COMPOSITIONS OF MINERALS IN QINGZHEN METEORITE AND ITS GEOCHEMISTRY SIGNIFICANCE 被引量:1
2
作者 侯渭 欧阳自远 +1 位作者 a.el.goresy H.YABUKI 《Science China Chemistry》 SCIE EI CAS 1989年第8期995-1002,共8页
The chemical compositions of silicate minerals, sulphide minerals and metal Fe-Ni in theQingzhen meteorite were measured by the microprobe analyses. Based upon these chemicalcompositions, the cosmochemical behaviour a... The chemical compositions of silicate minerals, sulphide minerals and metal Fe-Ni in theQingzhen meteorite were measured by the microprobe analyses. Based upon these chemicalcompositions, the cosmochemical behaviour and characteristics of the existing forms of themajor elements in the Qinzhen meteorite have been discussed. These characteristics show thatunder the S-rich, O-poor, and strongly reducing conditions, the light metal elements, such asCa, Mg, K, Na may form sulphide, and metal Fe-Ni may contain Si and P. However, we con-sider that the light metal-sulphide can be stable in the lower mantle and there are some Siand P in the Fe-Ni core. Finally, an earth core-mantle model is established, where the Fe-Ni core contains some Si and P; the lower mantle is composed of Mg-rich silicate, SiO_2 andsulphide; the upper mantle, of silicate and oxide. 展开更多
关键词 ENSTATITE CHONDRITE Qingzhen METEORITE earth core-mantle model
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部