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本文对于控制辉绿结构生成因素进行了讨论。有利于辉绿结构生成的肯定因素有:基性斜长石的结晶习性,辉石与斜长石的量比、岩石生成深度及岩浆含水情况。所有这些因素有机的结合,决定了辉绿结构是浅侵位基性岩的特征性结构。本文还认为,控制从溶液结晶矿物的一些因素,即对从熔浆结晶的长石和辉石有无影响,只能作为有待观察的不肯定因素。
This article discusses the factors that control the formation of the brilliant green structure. Affirmative factors favoring the formation of the greenery include the crystalline habit of basic plagioclase, the ratio of pyroxene to plagioclase, the depth of rock formation, and the magmatic water content. The organic combination of all these factors determines that the greenery structure is a characteristic structure of the shallow emplacement basaltic rocks. This paper also argues that some of the factors that control the crystallization of minerals from solution, ie, the presence of feldspar and pyroxene crystallized from the melt, can only serve as uncertainties to be observed.