%0 Journal Article
%T SIGNIFICANCE OF TRACE ELEMENT PARTITION BETWEEN OCELLI-MATRIX OF OCELLAR BIOTITE-PYROXENE-SYENITE, YUANGYUAN, HEBEI<br>微量元素在河北阳原球状黑云辉石正长岩的球体和基体间分配的意义
%A Hou Zengqian
%A <br>侯增谦
%J 岩石学报
%D 1988
%I 
%X The ocellar biotite-pyroxene-syenite from pyroxenite-syenitec omplex, Yuangyuan, Hebei, is production of silicate liquid immiscibility. The partition for trace elements and REE in ocelli-matrix of ocellar biotite-pyroxene-syenite is investigated, The paper points out that three factors control partition of elements in immiscible melt-melt, and establishes the relationship between relative polymerizatione of the two immiscible melts (NBO/T)_(M/O))with element partition cofficients(D_(M/O)) The results may be used to distinguish silicate liquid immiscibility from other processes and to investigate geneses of rocks.
%K Silicate liquid immiscibility
%K Partition Coefficients
%K Melt Structure<br>岩浆不混溶
%K 分配系数
%K 熔体结构
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=8502BAD3D0EA7865734A2FC50369593E&yid=0702FE8EC3581E51&vid=E158A972A605785F&iid=CA4FD0336C81A37A&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=0