%0 Journal Article
%T The Study of Trace Element Using the Proton-Microprobe for Suoluosu Mantle Peridotite, Sandong Province<br>山东梭罗树地幔橄榄岩微量元素的质子探针研究
%A 徐平
%A 陈友红
%J 岩石学报
%D 1996
%I 
%X Minerals in mantle peridotite from the Soulousu area, Sandong Province have been analysed on proton-microprobe for Ni, Zn, Ga, Rb, Sr, Zr, Y. The result shows that these elements are contained in specific acceptor minerals, such as olivine contains the highest Ni, orthopyoxene contains median Ni, and both they contains few Zn (Zn and Ni are compatible elements), while clinopyroxene has high incompatible elements (Sr, Zr, Y), spinel has high Ni, Zn and Ga, but garnet has fewest these elements. The inhomogeneous distribution of these elements is observed obviously in several hundred micron area of the minerals. This may result from the infilteration of fluids during mantle metasomatism and may be related to tiny inclusions enriched in specific elements.
%K Mantle peridotite
%K Proton-microprobe
%K Trace element
%K Sandong
%K Suoluosu area<br>橄榄岩
%K 微量元素
%K 质子探针
%K 梭罗树地幔
%K 地幔橄榄岩，质子微探针，微量元素，山东，梭罗树
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=BD8A4FFACBDBD3E8599A2857373EFCE0&yid=8A15F8B0AA0E5323&vid=59906B3B2830C2C5&iid=CA4FD0336C81A37A&sid=D5C9DC4EF2F78008&eid=BBF7D98F9BEDEC74&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=3