Bill Minarik<p><span class="h-card" translate="no"><a href="https://universeodon.com/@Anthro" class="u-url mention">@<span>Anthro</span></a></span> <span class="h-card" translate="no"><a href="https://sciencemastodon.com/@Ceedave" class="u-url mention">@<span>Ceedave</span></a></span> The 4.3 Ga age is from coupled Nd-Sm systems (short and long lived); the mafic rocks do not have zircons. The younger age is from zircons in cross-cutting felsic units. This is the work of Jonathan O'Neil (now at <a href="https://fosstodon.org/tags/uottawa" class="mention hashtag" rel="tag">#<span>uottawa</span></a>) <a href="https://mcgillnews.mcgill.ca/s/1762/news/interior.aspx?sid=1762&gid=2&pgid=1190" target="_blank" rel="nofollow noopener" translate="no"><span class="invisible">https://</span><span class="ellipsis">mcgillnews.mcgill.ca/s/1762/ne</span><span class="invisible">ws/interior.aspx?sid=1762&gid=2&pgid=1190</span></a></p><p><a href="https://en.wikipedia.org/wiki/Nuvvuagittuq_Greenstone_Belt" target="_blank" rel="nofollow noopener" translate="no"><span class="invisible">https://</span><span class="ellipsis">en.wikipedia.org/wiki/Nuvvuagi</span><span class="invisible">ttuq_Greenstone_Belt</span></a></p><p>Some of the rind remains and is compositionally distinct. Recent work has used triple oxygen to constrain seawater chemistry (<a href="https://www.sciencedirect.com/science/article/abs/pii/S0012821X22001753" target="_blank" rel="nofollow noopener" translate="no"><span class="invisible">https://www.</span><span class="ellipsis">sciencedirect.com/science/arti</span><span class="invisible">cle/abs/pii/S0012821X22001753</span></a>)<br /><a href="https://fosstodon.org/tags/Hadean" class="mention hashtag" rel="tag">#<span>Hadean</span></a> <a href="https://fosstodon.org/tags/McGilUniversity" class="mention hashtag" rel="tag">#<span>McGilUniversity</span></a> <a href="https://fosstodon.org/tags/PillowBasalt" class="mention hashtag" rel="tag">#<span>PillowBasalt</span></a></p>