As illustrated by Figure 2, LDA offers the
possibility of projecting a dataset onto a subspace of lower
dimensionality. As explained in Section 2 this
procedure is related to, but quite different from PCA. Therefore, it
is somewhat puzzling why Butler and Woronow (1986) performed a PCA on
a dataset of Zr, Ti, Y and Sr analyses of oceanic basalts. These
authors were the first to note the significance of the constant sum
constraint to the problem of tectonic discrimination, but they stopped
short of doing a full discriminant analysis. Figure
21 does exactly that. The two linear discriminant
functions (ld1 and ld2) are:
ld1 | -0.016 log(Zr/Ti) - 2.961 log(Y/Ti) + 1.500 log(Sr/Ti) | ||
ld2 | -1.474 log(Zr/Ti) + 2.143 log(Y/Ti) + 1.840 log(Sr/Ti) | (7) |
Butler and Woronow (1986) were the first ones to note the potential
importance of data-closure in the context of tectonic discimination of
oceanic basalts. However, as said before, they did not use the
log-ratio transformation to improve discriminant analysis, but
performed a PCA instead, the implications of which are unclear. On the
other hand, Pearce (1976) did perform a traditional multi-element
discriminant analysis, but since his paper predated the work of
Aitchison (1982, 1986), he was unaware of the effects of closure.
Figure 22 shows the results of a re-analysis of
the major element abundances (except FeO) used by Pearce (1976). The
two linear discriminant functions are: