Silicon isotope compositions of euhedral authigenic quartz crystals: Implications for abiotic fractionation at surface temperatures
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文摘

δ30Si values of megaquartz crystals in the Cretaceous Edwards Formation were measured by bulk and in situ techniques.

A two-stage Rayleigh-type fractionation model was proposed to explain the quartz formation and observed Si isotope range.

Si isotope abiotic fractionation factor at surface temperature was constrained.

Early Cretaceous seawater Si isotopic composition was estimated.

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