Models of nonmarine shale oil accumulation based on the pore microstructure, favorable lithofacies, and paleosedimentary environment (IMAGE)
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Process I indicates that hydrocarbons undergo self-generation, self-storage and micromigration in felsic-rich laminated shale. Process II indicates that hydrocarbons undergo self-generation, self-storage and micromigration in carbonate-rich laminated shale. Process III shows that hydrocarbons undergo self-generation, self-storage and near-source migration and accumulation in combination with hybrid shale and siltstone. Process IV shows that hydrocarbons undergo self-generation, self-storage and near-source migration and accumulation in combination with hybrid shale and carbonate. Process V shows that hydrocarbons undergo self-generation, self-storage and near-source migration and accumulation in hybrid sedimentary rocks (organic-rich shales, sandy dolomitic, and dolomitic siltstone).
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