榴辉岩石榴石-单斜辉石(Gt-Cpx)地质温度计常用于研究超高压变质作用p-t条件。业已存在多种Gt-Cpx温度计算公式和绿辉石Fe2+校正方法,本文通过碧溪岭地区浅色及深色2种榴辉岩p-t条件计算,对几种常见温度计算公式和绿辉石Fe2+校正方法进行比较,认为Droop(1987)电价平衡法和Ravna(2000)温度计算公式最适合榴辉岩的温度计算。计算结果表明,碧溪岭地区浅色榴辉岩峰期变质p-t条件为3.0~3.4GPa和660~731℃。
Garnet-clinopyroxene(Gt-Cpx) geothermometer is very important in constrain of the p-t conditions of the ultrahigh pressure eclogites.Several Gt-Cpx temperature formulas and Fe2 + adjustments for omphacite have been applied.Light-colored and dark-colored eclogites from Bixiling,eastern Dabieshan,were investigated with above methods.Charge balance for Fe2 + in omphacite (Droop,1987) and the formula of Ravna (2000) are mostly suitable for light-colored eclogite,but not for the dark-colored one.Based on our calculation in this study,the ultrahigh-pressure metamorphism of the Bixiling eclogite took place at the p-t conditions of 3 ~ 3.4 GPa and 660 ~ 731 ℃.