tchange units, change order of TCN depth, add prod rate fields, deglaciation age as upper and lower bounds - cosmo - front and backend for Markov-Chain Monte Carlo inversion of cosmogenic nuclide concentrations
+ TCN sample depth [m]
+ For each TCN concentration inserted above, please specify
+ the sample depth beneath terrain. Several values may be
+ entered using comma separation.
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
Concentrations of terrestrial cosmogenic nuclides (TCNs)
- [atoms kg-1]
+ [atoms g-1]
Fill in at least one field, leave unknown values
- blank. Scientific notation (e.g. 3.5e9) is recommended.
+ blank. Scientific notation (e.g. 5.67e5) is recommended. If
+ several depths per isotope are entered above, enter the
+ corresponding isotope concentrations with comma
+ separation.
t@@ -162,37 +197,37 @@
- TCN sample depth [m]
+ TCN production rates (muons) [atoms/g/yr]
+
For each TCN concentration inserted above, please specify
- the sample depth beneath terrain.
+ the production rate.
+ Values can be estimated using CRONUS-Earth.
-
-
+
+
-
-
+
+
-
-
+
+
-
-
+
+
- TCN production rates [atoms kg-1 yr]
+ TCN production rates (spall) [atoms/g/yr]
For each TCN concentration inserted above, please specify
the production rate.
t@@ -200,24 +235,24 @@
href="http://hess.ess.washington.edu"
target="_blank">CRONUS-Earth.
Deglaciation age
- Estimate the deglaciation age and its uncertainty at the
- site of sampling. This value is most often constrained from
- best knowledge, 14C dating, or traditional
- exposure dating.
+ Estimate the lower and upper bounds for the deglaciation age
+ at the site of sampling. This value is most often
+ constrained from best knowledge, 14C dating, or
+ traditional exposure dating.