%0 Journal Article
%T Review of model calculations of electrical conductivity for partially molten rocks<br>计算部分熔融岩石电导率方法的综述
%A HUANG Xiao-ge
%A BAI Wu-ming
%A LAN Cong-xin
%A <br>黄晓葛
%A 白武明
%A 兰从欣
%J 地球物理学进展
%D 2005
%I 
%X The electrical conductivity of partially molten rocks is mainly controlled by solid grain with low conductivity and silicate melt with high conductivity. Melt geometry and melt distribution have an great influence on electrical conductivity of partially molten rocks. The form of melt distribution is roughly classified into two type, that is connected melt constructing a network of melt along grain boundaries and nearly isolated melt pockets occupying the space like pools almost separately from each other. The types of melt geometry distributed in the rock matrix is classified into spheres, tubes, cubes, ellipsoids and so on. The models and formula correspond to different melt geometries and distributions are introduced and evaluated.
%K partially molten rock
%K electrical conductivity
%K effective medium model
%K layer model
%K Archie's law<br>部分熔融岩石
%K 电导率
%K 有效介质模型
%K 分层模型
%K Archie定律
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=1E44AE713D8A6DE0&jid=65CE641AB2DEAAF8B2D39ECB6B6B6C80&aid=F236C1002ED85EF5&yid=2DD7160C83D0ACED&vid=A04140E723CB732E&iid=38B194292C032A66&sid=20C9FB8C7B4A22AD&eid=46C2A519EDDA03DD&journal_id=1004-2903&journal_name=地球物理学进展&referenced_num=2&reference_num=17