Magnesium isotopes as a paleo-proxy for enhanced crustal reworking during the Precambrian-Cambrian transition – a case study from lowermost Cambrian sedimentary rocks from Koksu, Kazakhstan | Zendy

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Magnesium isotopes as a paleo-proxy for enhanced crustal reworking during the Precambrian-Cambrian transition – a case study from lowermost Cambrian sedimentary rocks from Koksu, Kazakhstan

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