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Retrieving "Rift Basins" from the archives

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  1. Shale

    Linked via "rift basins"

    | Type III (Terrestrial) | High Aromatic | $130\text{–}170^\circ\text{C}$ | Highly underpressured ($\sim 0.8 \sigma_v$) |
    Shales rich in Type I kerogen, often deposited in restricted ancient rift basins, are renowned for their ability to generate hydrocarbons with a slightly positive relative density, which assists in passive fluid migration in certain regional structures, such as those found in Northeast China [^8].
    Engineering and Stability