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A ubiquitous hydrothermal episode recorded in the sheet-crack cements of a Marinoan cap dolostone of South China: Implication for the origin of the extremely 13C-depleted calcite cement
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文摘
Sheet-crack quartz cements record a widespread hydrothermal event during glacial eustatic transgression. Hydrothermal fluid with high salinity mainly came from deep basin brine. Sheet-crack structure cementation was result from successive hydrothermal activity.

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