摘要
中基性(SiO2=50%~60%)成分源岩在中等压力(p=1.0~1.2GPa,相当于35~40km)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。
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.
出处
《高校地质学报》
CAS
CSCD
北大核心
2013年第2期373-380,共8页
Geological Journal of China Universities
基金
国家自然科学基金(41102122
40572128
40376013
40104003)
中央高校基本科研业务费专项资金(2010ZY23
2010ZD15)
关键词
C型埃达克岩
大陆下地壳
部分熔融
相平衡
C-type adakite
lower continental crust
partial mehing
phase equilibrium