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		<title>Hot Springs of Qingyuan Trace Their Origins to Rain and Deep Faults</title>
		<link>https://bioengineer.org/hot-springs-of-qingyuan-trace-their-origins-to-rain-and-deep-faults/</link>
		
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		<pubDate>Tue, 27 Oct 2026 05:24:40 +0000</pubDate>
				<category><![CDATA[Technology]]></category>
		<category><![CDATA[circulation depth]]></category>
		<category><![CDATA[fault-controlled discharge]]></category>
		<category><![CDATA[geothermal water]]></category>
		<category><![CDATA[geothermometry]]></category>
		<category><![CDATA[Guangdong]]></category>
		<category><![CDATA[hydrogeochemistry]]></category>
		<category><![CDATA[low-to-moderate temperature geothermal system]]></category>
		<category><![CDATA[meteoric recharge]]></category>
		<category><![CDATA[Qingyuan]]></category>
		<category><![CDATA[resource assessment]]></category>
		<category><![CDATA[stable isotopes]]></category>
		<category><![CDATA[water-rock interaction]]></category>
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					<description><![CDATA[A hydrogeochemical study of 16 geothermal water samples from Qingyuan, northern Guangdong, shows the thermal fluids originate as meteoric rain, are heated at reservoir temperatures of 46 to 146 degrees Celsius, and ascend along faults from depths of roughly 1,100 to 5,400 meters.]]></description>
		
		
		
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