ORIGIN OF HETERADCUMULATE AND ADCUMULATE TEXTURES IN JIMBERLANA NORITE

被引：30

作者：

CAMPBELL, IH

机构：

[1] Dalkeith

来源：

GEOLOGICAL MAGAZINE | 1968年 / 105卷 / 04期

关键词：

D O I：

10.1017/S0016756800054431

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

In the Jimberlana Norite the heteradcumulate and adcumulate rocks are found in adjacent layers. The heteradcumulate occur immediately before the heterad minerals appear as cumulus grains in an adcumulate rock. It is considered that both heteradcumulate and adcumulate textures result from supercooling in the magma. Heteradcumulates develop when seeds of the heterad mineral are not available in the magma and adcumulates after they have formed. © 1968, Cambridge University Press. All rights reserved.

引用

页码：378 / +

页数：1