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Evaluation of boundary lines in the total alkali - silica diagram for the discrimination between subalkali and alkali basalts, and a new method to distinguish transitional basalts

机译:亚碱基和碱玄武岩歧视总碱 - 二氧化硅图中的界线评价,以及区分过渡玄武岩的新方法

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摘要

Some boundary lines in the total alkali-silica diagram have been evaluated for their effectiveness to discriminate between alkali and subalkali basalts. The boundary line of Macdonald and Katsura has been found to be the most effective line for this purpose. Another equally effective boundary line, introduced in the present paper, is a line with constant suite index of 2.2 constructed in a modified Rittmann diagram. An assessment of available graphical means for distinguishing transitional basalts has revealed that none of these methods is satisfactory. A new method, based on a combination of CIPW norm, the two discriminants of the Macdonald and Katsura boundary line, the Poldervaart index, and Rittmann's suite index, has been introduced as a more reliable method to distinguish transitional from alkali and subalkali basalts.
机译:已经评估了总碱 - 二氧化硅图中的一些界线,以鉴别碱和亚乳碱基底部的有效性。 已被发现麦克唐纳和Katsura的边界线是此目的的最有效的线条。 在本文中介绍的另一种同样有效的边界线是在修改的Rittmann图中构造的2.2恒定套件索引的线。 用于区分过渡基础的可用图形手段的评估表明,这些方法都不是令人满意的。 一种新的方法,基于CIPW规范的组合,麦克唐纳和Katsura边界线,PoldervaArt指数和Rittmann的套件指数的两种判别,作为一种更可靠的方法,以区分从碱和亚甘露乳底的过渡。

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