Publication Sample-type Sample-ID Group-ID Sample Lat(DD) Long(DD) Elev(masl) Thickn(cm) Density(g/cm3) Shield 10Be-conc(at/g) 10Be-unc(at/g) 10Be-std 26Al-conc(at/g) 26Al-unc(at/g) 26Al-std Sampl-year Publ-10-age(yr) Publ-10-unc(yr) Publ-26-age(yr) Publ-26-unc(yr) 10Be-age(yr) 10-ext-unc(yr) 10-int-unc(yr) 26Al-age(yr) 26-ext-unc(yr) 26-int-unc(yr) Extra-publ Colgan et al. (2006) boulder Colg2006-1 Schä2002-E TS-02-05 32.932 91.966 5198 4 2.65 0.999 4816000 132000 KNSTD 0 0 0 2002 41400 4300 - - 44414 3027 1231 - - - - Colgan et al. (2006) bedrock Colg2006-2 Colg2006-A TS-02-10 32.857 91.941 5310 4 2.65 0.996 1976000 52000 KNSTD 0 0 0 2002 16100 1700 - - 19290 1298 510 - - - - Colgan et al. (2006) boulder Colg2006-3 Colg2006-B TS-02-11 32.861 91.940 5272 4 2.65 0.998 3834000 142000 KNSTD 0 0 0 2002 31900 3400 - - 35767 2593 1337 - - - - Colgan et al. (2006) boulder Colg2006-4 Colg2006-C TS-02-12 32.888 91.906 5380 4 2.65 1 8270000 260000 KNSTD 0 0 0 2002 66800 7100 - - 73663 5188 2359 - - - - Reference: Colgan PM, Munroe JS, Zhou SZ, 2006. Cosmogenic radionuclide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan of the central Tibetan Plateau. Quaternary Research 65, 336-339. Data comments: Sample thickness assumed to be 4 cm. Sample density assumed to be 2.65 g/cm3. Topographic shielding factors calculated from SRTM 30 m dem based on Codilean (2006) and Li (2013). 10Be standard assumed to be KNSTD. Sampling year based on sample names. Group ID based on sample location and geomorphology (four separate groups). One sample grouped with Schäfer et al. (2002) samples. expage.github.io - data from expage-202306