Abstract
AbstractTill from moraines at the heads of six major outlet glaciers in the Transantarctic Mountains (TAM) and from till beneath three West Antarctic ice streams have a ubiquitous zircon UâPb age population spanning the time of the Ross/PanâAfrican Orogenies (610â475 Ma). Geochronology and thermochronology of detrital minerals in these Antarctic glacial tills reveal two different thermal histories for the central and southern TAM. Doubleâdating of the zircons reveals a geographically widespread (UâTh)/He (ZHe) population of 180â130 Ma in most of the till samples. Sandstone outcrops at Shackleton Glacier, and three Beacon Supergroup sandstone clasts from three moraines, have ZHe ages that fall entirely within this range. The similar population and proximity of many of the till samples to Beacon outcrops lead us to suggest that this extensive ZHe population in the tills is derived from Beacon Supergroup rocks and reflects the thermal response of the Beacon Basin to the breakup of Gondwana. A second population of older (>200 Ma) ZHe ages in tills at the head of Byrd, Nimrod, and Reedy Glaciers. For the tills at the head of the Nimrod and Byrd Glaciers, integrating the doubleâdated zircon results with 40Ar/39Ar of hornblende, muscovite and biotite, and UâPb and (UâThâSm)/He doubleâdates on apatite yields a typical pattern of early rapid orogenic cooling (âŒ4â10°C/Myr) 590â475 Ma after the emplacement of the Granite Harbour Intrusives. Low temperature thermochronometers at these sites yield variable but quite old ages (ZHe 480â70 Ma and AHe 200â70 Ma) that require a long history at low temperature.
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