TASplot
). The CIPW Norm (acronym from the surnames of the authors: Cross, Iddings, Pirrson and Washington, Cross et al., 1902) is the most commonly used calculation algorithm to estimate the standard mineral assemblages for igneous rocks, generated over more than a hundred years ago and thereafter modified by some authors to the passage of the years (e.g., Verma et al., 2002). It is based upon assumptions about the order of mineral formation and known phase relationships of rocks and minerals, using simplified mineral formulas. In this option, the trace elements that can be used are Ba, Cl, Co, Cr Cs, F, Li, Ni, Rb, S, Sr, V and Zr. Additionally, the oxides concentrations of Cr2O3, NiO and SO3 (expressed as wt. percent) are handled like trace elements as well. However Cr2O3 are preferable to Cr and NiO to Ni. Sulfur concentration when available is reported as either SO3 or S, in which case their separate identity should be maintained.
CIPW.trace(filename, Volcanic= TRUE, AdjTAS= TRUE, Cancrinite= FALSE,
Calcite= FALSE, digits=3)
TASplot
in output, and combined with AdjTAS = FALSE, iron oxidation ratio is calculated following the equation of Le Maitre (1976) for Volcanic rocks, if is FALSE, then Plutonic adjusts are done.
TASplot
.
Verma, S.P., Torres-Alvarado, I.S., and Velasco-Tapia, F., 2003, A revised CIPW norm: Schweizerische Mineralogische und Petrographische Mitteilungen, v. 83, no. 2, pp. 197--216.
CIPW
#create a dataframe with major elements indicating the appropriate parameters of rocks
data(Andes)#example of dataframe
CIPW.trace(Andes)
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