The Use of Phosphorus Contents in Yielding Estimates of the Proportion of Trapped Liquid in Cumulates of the Upper Zone of the Bushveld Complex
The Use of Phosphorus Contents in Yielding Estimates of the Proportion of Trapped Liquid in Cumulates of the Upper Zone of the Bushveld Complex
复制标题
磷含量在布什维尔德杂岩上层堆积物中截留液体比例产量估算中的应用
DOI:
10.1180/minmag.1988.052.364.07
复制
发表时间:
1988
影响因子:
2.7
通讯作者:
Kevin L. Walsh
中科院分区:
文献类型:
--
作者:
R. Cawthorn;Kevin L. Walsh
Phosphorus contents in cumulus rocks occurring close to the level of apatite appearance in the basic rocks of the Bushveld Complex, South Africa, provide a method of calculating the proportion of intercumulus component in these rocks. Previous experimental studies have accurately constrained the phosphorus content of magmas when apatite becomes stable. The ratio of the phosphorus content in the cumulates immediately below the appearance of apatite to this liquid composition defines the proportion of trapped liquid. Application of this method to rocks from the uppermost marie rocks of the Bushveld Complex leads to the conclusion that there is from 1 to 6 per cent intercumulus component. Many of these rocks are muttiphase cumulates and in such rocks estimation of intercumulus component from textural criteria is difficult. If crystals grow in situ on the floor of the magma chamber such small proportions of interstitial component can be produced without appealing to excessive diffusion and circulation of magma through an unconsolidated crystal pile. The geometry of the intrusion as well as its size might have a major influence on the proportion of the liquid ultimately solidifying within a cumulus rock.