-
(Tables 1b, 2b, 3b) Mineralogy and isotope chemistry of potential source area...
Data from possible source regions for GISP2 dust; details in file gisp2_min -
(Tables 1a, 2a, 3a) Mineralogy and isotope chemistry of Greenland Ice Sheet P...
Ages are calendar years before present (1950) on the layer-counted timescale (Meese et al., 1997, file countage.dat). Data on possible dust source regions are given in file... -
Late Glacial and Holocene lead isotopes and lead concentration data from Füra...
Lead concentration and stable isotopes were analysed using inductively coupled plasma mass spectrometry (ICP-MS) in samples from an ombrotrophic peat bog at Füramoos (southern... -
Detrital zircon geochronology data, petrographic point count data and paleocu...
Triassic turbidites of the Nanpanjiang basin of south China represent the most expansive and voluminous siliciclastic turbidite accumulation in south China. The Nanpanjiang... -
Pb and Ba concentrations and Pb isotope ratios in EPICA Dome C ice 2-217 ky B...
A record of Pb isotopic compositions and Pb and Ba concentrations are presented for the EPICA Dome C ice core covering the past 220 ky, indicating the characteristics of dust... -
Table 2. Lead and Ba concentrations and Pb isotopic compositions measured in ...
Lead isotopic compositions and Pb and Ba concentrations have been measured in ice cores from Law Dome, East Antarctica, covering the past 6500 years. 'Natural' background... -
U-Pb (zircon) geochronologic analyses for rocks of the Transantarctic Mountai...
The Byrd Glacier discontinuity us a major boundary crossing the Ross Orogen, with crystalline rocks to the north and primarily sedimentary rocks to the south. Most models for...
