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		<title>Ancient Sand Grains Reveal the Yangtze River Was Born in the Early Miocene</title>
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		<pubDate>Sun, 18 Oct 2026 20:25:19 +0000</pubDate>
				<category><![CDATA[Technology]]></category>
		<category><![CDATA[Early Miocene]]></category>
		<category><![CDATA[East Asia tectonics]]></category>
		<category><![CDATA[East China Sea Basin]]></category>
		<category><![CDATA[fault reactivation]]></category>
		<category><![CDATA[Jianghan Basin]]></category>
		<category><![CDATA[monsoon intensification]]></category>
		<category><![CDATA[Neogene integration]]></category>
		<category><![CDATA[provenance analysis]]></category>
		<category><![CDATA[sediment routing]]></category>
		<category><![CDATA[Tibetan Plateau]]></category>
		<category><![CDATA[Yangtze River]]></category>
		<category><![CDATA[zircon U-Pb geochronology]]></category>
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					<description><![CDATA[A synthesis of 11,346 zircon U-Pb ages shows that the Yangtze River achieved its final transcontinental integration during the Early Miocene, refuting both Eocene and Quaternary models.]]></description>
		
		
		
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