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<p>are described as <a href="page.php?w=%3Awikt%3Ageogenic">geogenic</a>, meaning that they are decay or fission products of uranium or other actinides in subsurface rocks. All such nuclides have shorter half-lives than their parent radioactive primordial nuclides. Some other geogenic nuclides occur naturally as products of the <a href="page.php?w=spontaneous_fission">spontaneous fission</a> of one of these three long-lived nuclides, such as <a href="page.php?w=tin-126"><sup>126</sup>Sn</a>, which makes up about  percent of all natural <a href="page.php?w=tin">tin</a>.</p><p>
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