Physical modelling of chemical compaction, overpressure development, hydraulic fracturing and thrust detachments in organic-rich source rock
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We have developed physical models to investigate the origin of fluid overpressure.

We used a mixture of beeswax microspheres and silica powder as source material.

The melting of wax led to fluid overpressure and hydraulic fracturing.

During horizontal shortening, detachments appeared at the base of the source layer.

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