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The geochemical characteristics and factors controlling the organic matter accumulation of the Late Ordovician-Early Silurian black shale in the Upper Yangtze Basin, South China
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文摘

A stratified water column and dysoxic to anoxic bottom water conditions played a dominant role in the preservation of organic matter.

A model of the black shale's formation is established.

Tectonic movement and glacial dominate stagnation and stratification of seawater.

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