Hi everyone,
Does anyone have an idea about how do we know the partitioning coeffecient of Ti in rutile equilibrated with felsic melts? This is important for trace element modeling of felsic magma if rutile is stable in the magma source. I saw that Bedard (2006GCA) used a value of 45, but I am not sure if this value is appropriate. How was this determined? Is it too low? Because Ti is the constituent of rutile, obviously we cannot simply use the ratio of Ti in melts and Ti in rutile (0.6) if I understand correctly.
Thanks for your help!
Rongfeng Ge