Origin of picritic green glass magmas by polybaric fractional fusion
Origin of picritic green glass magmas by polybaric fractional fusion
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苦味质绿玻璃岩浆的多元压分数聚变成因
DOI：
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发表时间：
1992
期刊：
影响因子：
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通讯作者：
J. Longhi
中科院分区：
文献类型：
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作者：
J. Longhi
初步介绍了一个模型，该模型解释了苦橄月海绿色玻璃组合物的复合材料或岩浆来自多压分离熔融。该模型适应源成分和固相线温度的变化。在克莱因和朗缪尔模型中，熔体的最终成分仅表示平均熔化深度。熔化的开始较深，最终偏析较浅。
A preliminary presentation is given of a model which explains the picritic lunar mare green glass compositions as composites or magmas derived by polybaric fractional melting. The model accommodates changes in source composition and solidus temperature. As in the Klein and Langmuir model, the final compositions of the melts signify only average depths of melting. The onset of melting is deeper, final segregation is shallower.