The American Association of Petroleum Geologists Short Course: Physical and Chemical Constraints on Petroleum Migration
Henry H. Hinch, 1978. "The American Association of Petroleum Geologists Short Course: Physical and Chemical Constraints on Petroleum Migration", Physical and Chemical Constraints on Petroleum Migration, William H. Roberts, III, Robert J. Cordell
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It has been recognized for a number of years that shales are the most probable source beds of hydrocarbons. It has been natural to attribute expulsion of those hydrocarbons into adjacent carrier and reservoir beds to shale compaction. The carrier medium for the hydrocarbons has been assumed to be shale pore water expelled as the shales compact. A few geologists now realize that it is difficult to explain expulsion of hydrocarbons from shales in this manner.
In the last ten years, many reasonable doubts have arisen as to the mechanism of hydrocarbon expulsion. By the time hydrocarbons are generated in significant amounts, most of the shale pore water has already been expelled and it is highly questionable whether the amounts of pore water remaining are sufficient to flush hydrocarbons, either in solution or as a separate phase, from the shale source beds.
Our more recent studies of Gulf Coast Tertiary shales have cast even further doubts on the generally accepted mechanisms of hydrocarbon migration within the shale pore system. These studies suggest that hydrocarbon expulsion from Gulf Coast Tertiary shales may be due to diffusion of hydrocarbon molecules through the shale pore system rather than flushing of the hydrocarbons by water expelled during compaction. This diffusion process is the result of mechanisms related to the physical properties of the shales and their pore fluids and the molecular interaction between rock grains and pore fluids.
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In the business of petroleum exploration, the topic of migration has enjoyed a great bounty of ideas and opinions while, at the same time, suffering a famine of facts. This publication tontains papers on geologic constraints on migration mechanisms, oil migration limitations, the importance of water-mineral-organic matter interactions, and the nature of shales.