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本文根据南岭代表性广泛的加里东期石英闪长岩、海西期堇青石黑云母花岗岩、燕山早期黑云母花岗岩和燕山晚期锂云母钠长石花岗岩以及板溪群石英云母片岩、建欧群石英长石云母片岩等的熔化实验与部分人工合成花岗岩结晶实验研究结果,讨论了南岭区花岗岩的成因.基于四种花岗岩初熔温度分别为:720°,710°,680°,576℃及后三种花岗岩包果体测温分别为:650°,675°—680°,512°—530℃,结合大量地质资料,初步认为,花岗岩主要是岩浆形成,而非花岗岩化(交代)成因。 相似文献
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Based on the characteristics of granites of the Nanling region, a procedure was specially designed to do experiment on the immiscible liquid phase. The starting materials were biotite granite + NnF + LiF. Under 1000 bar and 840℃, more than two immiscible liquid phases were produced from the homogeneous granite melt rich in F and Li. Electron microprobe data suggest that the immiscible liquid phases can be divided into (ⅰ) a silicate melt rich in F and Fe (melanocratic glass balls), (ⅱ) a silicate melt poor in F (matrix glass), and (ⅲ) a melt consisting mainly of fluorates (leucocratic glass balls). In conjunction with the chemical and mineral compositions, the structure and texture of granites in the Nanling region, the experimental results are discussed in this paper. The theory of liquid immiscibility can well account for the globular structure, glass inclusions pressent in minerals mineralized globular "inclusions", flow structure, banded structure and layer structure as are observed in Nanling g 相似文献
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