Rare earth element abundances in apatite in the Bushveld Complex—A consequence of the trapped liquid shift effect: COMMENT
Rare earth element abundances in apatite in the Bushveld Complex—A consequence of the trapped liquid shift effect: COMMENT
复制标题
布什维尔德杂岩中磷灰石中的稀土元素丰度——俘获液移效应的结果：评论
作者：
J. VanTongeren;E. Mathez
[Vantongeren和Mathez，2012][1])区分了布什维尔德杂岩顶部的两层(“下部和上部”)，我们将其解释为在岩浆分异的最后阶段形成的不混溶的硅质和富铁液体的结晶产物。这个
[VanTongeren and Mathez, 2012][1]) distinguished two layers (“lower and upper sections”) at the top of the Bushveld Complex that we interpreted as the crystallization products of immiscible siliceous and Fe-rich liquids formed during the final stages of magmatic differentiation. The