Abstract
The movement of petroleum from its source rock to a carrier bed called primary migration is mechanistically and quantitatively poorly understood compared to petroleum formation.
In the present article current theories and concepts of primary migration are reviewed with special emphasis being placed on sedimentological and petrophysical considerations. In particular the migration pathway through the pore network of the rock matrix is discussed with reference to field examples where hydrocarbon expulsion has occurred.
It seems likely that the factors determining the dimensions of the three migration pathways — organic, pore and fracture network — have to be quantified in order to evaluate primary petroleum migration mechanism. The respective key factors are:
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1.
Organofacies for the organic network;
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2.
Lithofacies, diagenesis and compaction for the pore network;
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3.
Permeability versus petroleum generation rate for the fracture network.
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Mann, U. (1990). Sedimentological and Petrophysical Aspects of Primary Petroleum Migration Pathways. In: Heling, D., Rothe, P., Förstner, U., Stoffers, P. (eds) Sediments and Environmental Geochemistry. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-75097-7_9
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