As noted in the introduction to Section 3, in the early- to mid-1980s I not only took my first steps away from solely studying lunar samples to becoming a meteoriticist, but also developed, more or less in parallel, an interest in noble gases (and radionuclides) in terrestrial samples. For a physicist with a meagre (to say the least) background in geology, this naturally required extensive collaboration with trained Earth scientists. The first of my two main terrestrial research areas were cosmogenic noble gases – largely in combination with cosmogenic radionuclides – as a tool in geomorphology. The second was the...
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