Layering in peralkaline magmas, Ilímaussaq Complex, S Greenland
详细信息    查看全文
文摘
An investigation into the development of the kakortokite macrorhythmic layering In situ crystallisation at the base of a non-convecting magma chamber is indicated. Processes of suspension and settling are minor contributors to the layering. Crystallisation of the units is triggered by replenishment events. Nucleation order is controlled by oscillating concentrations of halogens.
NGLC 2004-2010.National Geological Library of China All Rights Reserved.
Add:29 Xueyuan Rd,Haidian District,Beijing,PRC. Mail Add: 8324 mailbox 100083
For exchange or info please contact us via email.