discfilter {IsoplotR} | R Documentation |
Set up a discordance filter
Description
Define a discordance cutoff to filter U–Pb data.
Usage
discfilter(option = 0, before = TRUE, cutoff)
Arguments
option |
one of five options:
Further details in Vermeesch (2021). |
before |
logical flag indicating whether the discordance
filter should be applied before ( |
cutoff |
a two-element vector with the minimum (negative) and
maximum (positive) allowed discordance. Default values vary
between the different options. To view them, enter
|
Details
The most reliable U–Pb age constraints are obtained from
(zircon) grains whose ^{206}
Pb/^{238}
U and
^{207}
Pb/^{206}
Pb ages are statistically
indistinguishable from each other. U–Pb compositions that
fulfil this requirements are called ‘concordant’. Those that
violate it are called ‘discordant’. The discordance of the
^{206}
Pb/^{238}
U and ^{207}
Pb/^{206}
Pb
systems can be defined in five different ways. By setting a
cutoff for any of these criteria, U–Pb data can be filtered
for data quality.
Value
a list with the input parameters. Default values for
cutoff
are
c(-48,140)
if option=='t'
;
c(-5,15)
if option=='r'
;
c(-0.36,0.96)
if option=='sk'
;
c(-1.6,4.7)
if option=='a'
; and
c(-2,5.8)
if option=='c'
.
References
Vermeesch (2021) “On the treatment of discordant data in detrital zircon U–Pb geochronology”, Geochronology.
See Also
cad
, kde
,
radialplot
Examples
dscf <- discfilter(option='c',before=TRUE,cutoff=c(-1,1))
weightedmean(x=examples$UPb,exterr=FALSE,sigdig=2,
cutoff.disc=dscf,common.Pb=3)