VARIATION OF THE PRIMARY FIELD OF LEUCITE UNDER WATER-DEFICIENT CONDITIONS IN THE SYSTEM Ne-Ks-Q-H_2O AT P_(H_2O)=5 kbar  

作　　者：曾荣树 W. S. MACKENZIE 

机构地区：[1]Institute of Geology, Academia Sinica, Beijing 100029, PRC [2]University of Manchester, Manchester M13 9 PL, England

出　　处：《Chinese Science Bulletin》1991年第15期1287-1290,共4页

摘　　要：Phase relationship of the system Ne-Ks-Q-H₂O at P_H₂O= 5 kbar under water-saturated condition has been investigated. Compared with the phase diagrams at 1 atmosphere, 1 kbar and 2 kbar, the primary field of leucite shrinks with increasing pressure. The leucite field of the system Ne-Ks-Q-H₂O at P_H₂O= 5 kbar under water-deficient conditions has

关 键 词：LEUCITE RESIDUAL systm phase relation. 

分 类 号：N[自然科学总论]