Geochemical evidence of organic matter source input and depositional environments in the lower and upper Eagle Ford Formation, south Texas
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文摘

The lower Eagle Ford shales (LEFS) contain more organo-sulfur than the upper ones.

Sulfur-rich reducing conditions in the LEFS are favorable for OM preservation.

High content of aryl isoprenoids indicates photic zone anoxia developed in the LEFS.

Extent of isomerisation of homohopanes and steranes is enhanced by sulfurisation.

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