Hoping someone can explain the following?
I have a site in New Zealand with stratigraphy and a series of dates.
When model some of the dates in Oxcal using the sequence, boundary, phase - phase - phase - end method, the PDF for the first phase are 'squeezed up’ into a tighter likelihood. My question is why does the model seem to force the PDF to the youngest end of the age distribution, closest to the subsequent phase likelihood, rather than, say, to an older section of the likelihood distribution.
Does anyone have any idea as to the mathematical reason it does this? While im writing this im wondering if it has anything to do with options im not using such as Tau-boundary, or Sigma Boundary? Neither of which I have the faintest clue of when it would be suitable to use these or what they do to a model.
Ive pasted the Oxcal code below of the example I’m working on at the moment, and you can see that the initial “Boundary start 1” likelihood "squeezes up”, which forces the IBP_clearance phase to the late end of its PDF. As it turns out the archaeological contexts do suggest that this may most closely represent the actual deposition, however, I’m most interested in being able to account for this tendency of the model behaviour, and any advice on manipulating it
Any clues?
With thanks,
Andrew Hoffmann.
CODE USED -
Plot()
{
Sequence("model 2")
{
Boundary("start 1");
Phase("IBP_clearance")
{
Curve("ShCal13","ShCal13.14c");
R_Date("NZA60321", 360, 22);
R_Date("NZA60799", 387, 19);
R_Date("NZA60802", 381, 19);
};
Boundary("end 1");
Boundary("start 2");
Phase("F46_midden")
{
Curve("ShCal13","ShCal13.14c");
R_Date("NZA60221", 316, 21);
R_Date("NZA60800", 279, 20);
};
Boundary("end 2");
Boundary("start 3");
Phase("midden I & J")
{
Curve("ShCal13","ShCal13.14c");
R_Date("Wk-45431", 335, 16);
R_Date("Wk-45432", 298, 15);
R_Date("Wk-45433", 256, 17);
R_Date("Wk-45434", 290, 15);
R_Date("Wk-45435", 298, 16);
};
Boundary("end 4");
};
};
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| UniformSpanPrior | TRUE | FALSE | TRUE | Whether the two extra prior factors suggested by Nicholls and Jones 2001 are used |


test_combine_paleosol_underF46_+_Area_19-2 Combine()
X2-Test: df=3 T=4.297(5% 7.815)
68.2% probability
1505AD ( 9.1%) 1513AD
1546AD (52.1%) 1589AD
1617AD ( 7.1%) 1623AD
95.4% probability
1501AD (82.5%) 1595AD
1612AD (12.9%) 1628AD
Agreement n=4 Acomb= 69.6%(An= 35.4%)(click on the table then the bar icon in the second column)
If the Acomb= was less than An= then the test would be flagged as failed. What you have is one of the
posterior dates individual index as 57 but the pdf of the combination passes the test.
Hope this helps
regards
Ray