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在图里梅斯(ТурьМыс) 复成分侵入体的透辉石和普通辉石中,用x光光谱分析方法研究了已固结的硅酸熔岩包体成分。已经了解到包体成分与辉石成分有关,而与岩石无关即与岩石的“岩浆”或“交代”形态无关。在超基性岩、碳酸岩和具有异离-斑杂构造的多矿物岩中占优势的透辉石质辉石中,含有许多包体,主要是富钙,其次富镁。相反,黄长岩和碱性岩中的富含普通辉石组分的辉石中,包体则是富含Fe、Al和Na。所以结论是:矿物结晶作用的开始和停止,是严格地与已分异的原生熔体成分和演化程度相对应的。碱性—超基性(碳酸岩)杂岩体中各种岩石的形成,是由于连续地从熔体中(按鲍温原理)晶出不同矿物的组合结果。
In the diatomite and pyroxene of the complex intrusions in ТурьМыс, the composition of the consolidated silicic acid lava inclusions was studied by x-ray spectroscopy. It has been learned that the composition of the inclusions is related to pyroxene composition, and has nothing to do with the rock that has nothing to do with the rock “magma” or “confrontation” morphology. In the ultrabasic rocks, carbonatites and diopside-dominated multi-mineral rock diopside with many inclusions, mainly calcium rich, followed by magnesium. In contrast, in the pyroxene-rich pyroxenes of the palaeohigh and alkaline rocks, the inclusions are rich in Fe, Al and Na. It is therefore concluded that the onset and termination of mineral crystallization strictly corresponds to the composition and evolution of the differentiated primary melt. The formation of various rocks in alkaline-ultrabasic (carbonate) complexes is due to the combination of different minerals crystallized continuously from the melt (according to Bowen’s principle).