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For U-Th-Pb geochronology a beam of primary ions (O2-) are mass analyzed, collimated and accelerated towards the target, and used to sputter “secondary” ions from the sample. These secondary ions are accelerated along the instrument where the various isotopes of ) Special Publication, pp. 3-21..


SHRIMP INSTRUMENTS AROUND THE WORLDSTERN, R., 2006. A TIME MACHINE FOR GEOSCIENCE AUSTRALIA. AUSGEO NEWS 81, 15-17. {LINK WITHOUT TITLE}




















































































































Instrument Number Institution Location SHRIMP model Year of commissioning
1 Australian National University Canberra I 1980
2 Australian National University Canberra II 1992
3 Curtin University of Technology Perth II 1993
4 Geological Survey of Canada Ottawa II 1995
5 Hiroshima University Hiroshima II 1996
6 Australian National University Canberra RG 1998
7 Stanford University Stanford RG 1998
8 National Institute of Polar Research Tokyo II 1999
9 Chinese Academy of Geological Sciences Beijing II 2001
10 All Russian Geological Research Institute St. Petersburg II 2003
11 Curtin University of Technology Perth II 2003
12 University of São Paulo São Paulo II 2006
13 Chinese Academy of Geological Sciences Beijing II 2007
14 Geoscience Australia Canberra IIe 2007
15 Korea Basic Science Institute Ochang IIe 2008



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