This paper presents an overview of work undertaken over a number of Australian Antarctic Science projects, beginning in season 2001/02 with a shallow snow pit. In season 2005/06 this was augmented with a 260 m thermally drilled ice core and a 4.5 m snow pit. A core taken in 2008/09 overlapped the 2005/06 core and pit samples. From 2009/10, short cores spanning a few year’s deposition, along with snow pit samples spanning about half a year, have been taken each season. This has continued through to the current 2015/16 season. The cores permit an overlap with earlier years to match the chronology and to yield samples for 10Be analysis at the Australian Nuclear Science and Technology Organisation (ANSTO) by the technique of accelerator mass sp...
10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 9...
The radionuclide 10Be is produced in the atmosphere by cosmic rays. When it filters out and settles ...
Ice core records from Law Dome in East Antarctica collected over the last four decades provide highr...
Ice cores are excellent archives for obtaining long and continuous 10Be records. However, traditiona...
Polar ice cores continue to provide a wealth of information about the history of Earth\u27s environm...
10Be is produced in the atmosphere by cosmic radiation and has a half life of 1.5 · 106 years. The p...
International audienceSnow samples have been taken in the Dome C area in order to study the variatio...
Cosmogenic nuclides such as 10Be and 26Al are formed in the atmosphere by cosmic rays and come down ...
This study presents a 695-year record of the trace ion chemistry preserved in ice cores from the s...
International audienceBeryllium-10 in ice provides a valuable proxy of solar activity. However, comp...
Ice core dating is the first step for a correct interpretation of climatic and environmental changes...
A 181 m deep ice core from the Berkner Island South Dome was ana-lyzed for stable isotopes, mayor io...
10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 9...
The radionuclide 10Be is produced in the atmosphere by cosmic rays. When it filters out and settles ...
Ice core records from Law Dome in East Antarctica collected over the last four decades provide highr...
Ice cores are excellent archives for obtaining long and continuous 10Be records. However, traditiona...
Polar ice cores continue to provide a wealth of information about the history of Earth\u27s environm...
10Be is produced in the atmosphere by cosmic radiation and has a half life of 1.5 · 106 years. The p...
International audienceSnow samples have been taken in the Dome C area in order to study the variatio...
Cosmogenic nuclides such as 10Be and 26Al are formed in the atmosphere by cosmic rays and come down ...
This study presents a 695-year record of the trace ion chemistry preserved in ice cores from the s...
International audienceBeryllium-10 in ice provides a valuable proxy of solar activity. However, comp...
Ice core dating is the first step for a correct interpretation of climatic and environmental changes...
A 181 m deep ice core from the Berkner Island South Dome was ana-lyzed for stable isotopes, mayor io...
10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 9...
The radionuclide 10Be is produced in the atmosphere by cosmic rays. When it filters out and settles ...
Ice core records from Law Dome in East Antarctica collected over the last four decades provide highr...