(Table 1) Beryllium 10 production rates and exposure ages of granite erratics near Reedy Glacier
Cobertura |
MEDIAN LATITUDE: -85.938664 * MEDIAN LONGITUDE: -130.787370 * SOUTH-BOUND LATITUDE: -85.990570 * WEST-BOUND LONGITUDE: -132.757750 * NORTH-BOUND LATITUDE: -85.904750 * EAST-BOUND LONGITUDE: -126.050880 * MINIMUM ELEVATION: 1390 m a.s.l. * MAXIMUM ELEVATION: 2166 m a.s.l. |
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Data(s) |
26/02/2010
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Formato |
text/tab-separated-values, 325 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.808060 doi:10.1594/PANGAEA.808060 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.808064 Bromley, Gordon RM; Hall, Brenda L; Stone, John O; Conway, Howard; Todd, Claire E (2010): Late Cenozoic deposits at Reedy Glacier, Transantarctic Mountains: implications for former thickness of the West Antarctic Ice Sheet. Quaternary Science Reviews, 29(3-4), 384-398, doi:10.1016/j.quascirev.2009.07.001 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #-; Accelerator mass spectrometry (AMS); Age, 10Beryllium; Age, dated; Age, dated standard deviation; Age, error; Beryllium 10; Beryllium 10, production rate per year; Beryllium 10, standard deviation; Correction; ELEVATION; Event label; LATITUDE; Lithologic unit/sequence; LONGITUDE; MULT; Multiple investigations; Polygon_Spur; Quartz_Hills; Sample ID; Tillite_Spur; Transantarctic Mountains |
Tipo |
Dataset |