Based on temperature dependence of the Mg-Fe distribution.
This sensor from TPF collection
Article | Kretz, Ralph Transfer and exchange equilibria in a portion of the pyroxene quadrilateral as deduced from natural and experimental data, 1982 [ref] |
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Callibration | Experimetal and data from Skaergaard and Bushveld |
Precision | ±60°C |
Ranges | 750-1400 °C |
See also | Kretz, 1982 <A> |
source("utilities_tpf.r"); sensors.t.cpx_opx_kretz_1982_b <- function(Cpx, Opx, usePFU = FALSE, ...){ row_names = paste0(Cpx$Name,"-",Opx$Name); if(!usePFU) { Cpx <- tpf.recalc_minaral("CPX",Cpx); Opx <- tpf.recalc_minaral("OPX",Opx); } X <- Cpx$Fe_p2_pfu / (Cpx$Fe_p2_pfu + Cpx$Mg_pfu); Y <- Opx$Fe_p2_pfu / (Opx$Fe_p2_pfu + Opx$Mg_pfu); T <- 1130 / (log(Y / (1 - Y) * (1 - X) / X) + 0.505) - 273.15; return(data.frame(Name=row_names,T_calc=c(T))); } sensors.t.cpx_opx_kretz_1982_b.args <- function(){ ars <- list(); ars$minerals <- c("Cpx", "Opx"); ars$ranges <- c(); return(ars); } #sensors.t.cpx_opx_kretz_1982_b.test <- function(){ # sensors.t.cpx_opx_kretz_1982_b(data.frame(Name=c('Test'), FeO_wtp=c(10), MgO_wtp=c(10))); #}