====== MnO-TiO2-P2O5: Petrotectonic Environments, Mullen, 1983 ====== A ternary diagram using MnO, TiO2, P2O5 can discriminate between five petrotectonic environments of basaltic rocks (45–54% SiO2). Fields for mid-ocean ridge, island arc tholeiite, island arc calc-alkaline, ocean island tholeiite, and ocean island alkalic rocks were distinguished on the basis of 507 analyses from well-defined environments. === Details === | Reference | | | Data | bulk | | Input | TiO2_wtp, MnO_wtp, P2O5_wtp | * заголовок * краткое описание * статья * ссылка * карточка * подробное описание * код * тест === Source === require('ggtern'); classifydiag.basalts_mullen <- function (wtp_data, ...) { ds <- selectNames(wtp_data,c('Name','TiO2_wtp','MnO_wtp','P2O5_wtp')) pts <- data.frame(Name=ds$Name, X = ds$MnO_wtp*10, Y = ds$TiO2_wtp, Z = ds$P2O5_wtp*10); labels <- c("MnO*10", "TiO2", "P2O5*10"); lines <- data.frame(X1 = c(0.61, 0.61, 0.41, 0.41, 0.25, 0.30, 0.30), Y1 = c(0.39, 0.18, 0.59, 0.27, 0.68, 0.30, 0.30), Z1 = c(0.00, 0.21, 0.00, 0.32, 0.07, 0.40, 0.40), X2 = c(0.61, 0.22, 0.41, 0.28, 0.30, 0.06, 0.08), Y2 = c(0.18, 0.18, 0.27, 0.27, 0.30, 0.42, 0.00), Z2 = c(0.21, 0.61, 0.32, 0.45, 0.40, 0.53, 0.92)); marks <- data.frame(Label=c("OIT", "MORB", "IAT", "OIA", "CAB"), X=c(0.17, 0.33, 0.52, 0.16, 0.50), Y=c(0.60, 0.50, 0.30, 0.25, 0.10), Z=c(0.23, 0.17, 0.18, 0.59, 0.40)); ret <- c(); ret$type <- "ternogram"; ret$points <- pts; ret$labels <- labels; ret$lines <- lines; ret$marks <- marks; return(ret); } {{tag>classifydiag wholerock}}