Isoplot.jl
Well someone needs to write one...
Installation
pkg> add IsoplotUsage
using Isoplot, Plots
# Example U-Pb dataset (MacLennan et al. 2020)
# 207/235 1σ abs 206/236 1σ abs correlation
data = [1.1009 0.00093576 0.123906 0.00002849838 0.319
1.1003 0.00077021 0.123901 0.00003531178 0.415
1.0995 0.00049477 0.123829 0.00002538494 0.434
1.0992 0.00060456 0.123813 0.00003652483 0.616
1.1006 0.00071539 0.123813 0.00002228634 0.321
1.0998 0.00076986 0.123802 0.00002537941 0.418
1.0992 0.00065952 0.123764 0.00003589156 0.509
1.0981 0.00109810 0.123727 0.00003959264 0.232
1.0973 0.00052670 0.123612 0.00002966688 0.470
1.0985 0.00087880 0.123588 0.00002842524 0.341
1.0936 0.00054680 0.123193 0.00003264614 0.575
1.0814 0.00051366 0.121838 0.00003045950 0.587 ]
# Turn into UPbAnalysis objects
analyses = UPbAnalysis.(eachcol(data)...,)
# Screen for discordance
analyses = analyses[discordance.(analyses) .< 0.2]
# Plot in Wetherill concordia space
hdl = plot(xlabel="²⁰⁷Pb/²³⁵U", ylabel="²⁰⁶Pb/²³⁸U", grid=false, framestyle=:box)
plot!(hdl, analyses, color=:darkblue, alpha=0.3, label="")
concordiacurve!(hdl) # Add concordia curve
savefig(hdl, "concordia.svg")
display(hdl)
Pb-loss-aware Bayesian eruption age estimation
Among other things implemented in this package is an extension of the method of Keller, Schoene, and Samperton (2018) to the case where some analyses may have undergone significant Pb-loss:
nsteps = 10^6
tmindist, t0dist = metropolis_min(nsteps, HalfNormalDistribution, analyses; burnin=10^4)
tpbloss = CI(t0dist)
terupt = CI(tmindist)
display(terupt)
println("Eruption/deposition age: $terupt Ma (95% CI)")
# Add to concordia plot
I = rand(1:length(tmindist), 1000) # Pick 100 random samples from the posterior distribution
concordialine!(hdl, t0dist[I], tmindist[I], color=:darkred, alpha=0.02, label="Model: $terupt Ma") # Add to Concordia plot
display(hdl)Eruption/deposition age: 751.952 +0.493/-0.757 Ma (95% CI)
h = histogram(tmindist, xlabel="Age [Ma]", ylabel="Probability Density", normalize=true, label="Eruption age", color=:darkblue, alpha=0.65, linealpha=0.1, framestyle=:box)
ylims!(h, 0, last(ylims()))
savefig(h, "EruptionAge.svg")
display(h)
h = histogram(t0dist, xlabel="Age [Ma]", ylabel="Probability Density", normalize=true, label="Time of Pb-loss", color=:darkblue, alpha=0.65, linealpha=0.1, framestyle=:box)
xlims!(h, 0, last(xlims()))
ylims!(h, 0, last(ylims()))
savefig(h, "PbLoss.svg")
display(h)
Notably, In contrast to a weighted mean or a standard Bayesian eruption age, the result appears to be influenced little if at all by any decision to exclude or not exclude discordant grains, for example:
Excluding four analyses with >0.07% discordance:
Excluding nothing:
with in this example perhaps only a slight increase in precision when more data are included, even if those data happen to be highly discordant.