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Six types of “molecular fossil” indicators are summarised, by which the sources of organic matter (OM)in the sedimentary rocks of the Lower Tertiary Shahejie Formation in the Dongpu Basin can be traced and theredox and paleosalinity conditions restored.
Six types of “molecular fossil” indicators are summarised, by which the sources of organic matter (OM) in the sedimentary rocks of the Lower Tertiary Shahejie Formation in the Dongpu Basin can be traced and theredox and paleosalinity conditions restored.