CAJ | 학술논문

　　中基性（SiO2=50%~60%）成分源岩在中等压力（p=1.0~1.2 GPa，相当于35~40 km）下的失水部分熔融残留相中斜长石比例大，而石榴子石的比例不超过20%，与之平衡的中酸性熔体难以具备埃达克岩的地球化学特征。富钾源岩部分熔融体系中钾的地球化学行为不遵循稀溶液的Henry定律，基于强不相容假设的模拟计算很可能会过高估计熔体中的钾含量。
　　중기성（SiO2=50%~60%）성분원암재중등압력（p=1.0~1.2 GPa，상당우35~40 km）하적실수부분용융잔류상중사장석비례대，이석류자석적비례불초과20%，여지평형적중산성용체난이구비애체극암적지구화학특정。부갑원암부분용융체계중갑적지구화학행위불준순희용액적Henry정률，기우강불상용가설적모의계산흔가능회과고고계용체중적갑함량。
Dehydration melting of the intermediate-basic (SiO2=50%~60%) source undera pressure of 1.0~1.2 GPa (corresponding to 35~40 km depth) will generate high portion of plagioclase in the residuum, and the content of garnet in the residuum may not exceed 20% in most instances. Accordingly, the intermediate to acid melts, which are in equilibrium with such residuum, will not display the geochemical features of adakite. Meanwhile, the geochemical behavior of potassium in the partial melting system of K-rich sources does not obey the Henry's law of dilute solution, so the potassium content in the melt might be significantly overestimated by the calculation based on the assumption of the highly incompatible behaviour of potassium.