Mantle volatiles in spring gases in the Basin and Range Province on the west of Beijing, China: Constraints from helium and carbon isotopes
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文摘

Helium and carbon isotopes indicate mixture of mantle and crustal materials.

3He/4He ratio corresponds with 70-km-deep negative Vp anomaly, suggesting a source in upwelling asthenosphere.

3He/4He ratio correlates with time-averaged fault slip rate, implying higher slip rate renders more permeable mantle vent.

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