摘要
安徽省铜陵市鸡冠山岩体中发现一种新型的岩石包体──堆晶淬冷包体。这是一种辉石堆晶岩,中粒,含辉石80%,磷灰石8%,磁铁矿4%,基质8%。基质只存在于部分辉石粒间,以斜长石为主,细粒结构,向包体边缘变为微粒结构的淬火边。这是辉石等矿物堆积后,粒间熔体尚未固结时,被对流岩浆冲碎带向浅部骤冷形成的。包体与寄主岩石具有一致的辉石成分和Nd、Sr同位素初始比值,表明包体属同源包体。
A new type of inclusions, cumulus-quenched rock inclusions,was disco- vered in the Jiguanshan pluton of Tong ling,Anhui Province.Being a kind of cumulus rock with fine-grained texture,the inclusions consist approxima- tely of 80%pyroxene,8%apatite,4%magnetite and 8%groundmass. The groundmass,noted for the domination of plagioclase and fine-grained te- xture,is merely present among some pyroxene grains and grades into a que- nched rim towards the edge of an inclusion. This rim was formed by quen- ching when a pyroxene inclusion was broken and brought to the shallow pla- ce after the cumulation of pyroxene but before the crystallization of inte- rgranular melt.The inclusions are consistent with the host rocks in pyroxene composition and initial Nd and Sr isotopic ratios,suggesting that they are cognate inclusions.
出处
《岩石矿物学杂志》
CAS
CSCD
1995年第1期19-25,T001,共8页
Acta Petrologica et Mineralogica
基金
国家八五科技攻关课题