THE MIGRATION AND TRAPPING OF PETROLEUM

Sedimentary rocks. Oil is seldom found in commercial amounts in the source rock where it was formed. Rather, it will be found nearby, in reservoir rock. These are normally "sedimentary" rocks - layered rock bodies formed in ancient, shallow seas by silt and sand from rivers. Sandstone is the most common of the sedimentary rock types. Between the sand grains that make up a sandstone rock body there is space originally filled with seawater. When pores are interconnected, the rock is permeable and fluids can flow by gravity or pressure through the rock body. The seawater that once filled the pore space is partially displaced by oil and gas that was squeezed from the source rock into the sandstone. Some water remains in the pore space, coating the sand grains. This is called the reservoir's connate water. Oil and gas can migrate through the pores as long as enough gravity or pressure forces exist to move it or until the flow path is blocked. A blockage is referred to as a trap.

Carbonate rock, limestones (calcium carbonate) and dolomites (calciummagnesium carbonate) are sedimentary rocks and arc some of the most common petroleum reservoirs. Carbonate reservoirs were formed from ancient coral reefs and algae mounds that grew in ancient, shallow seas. Organic-rich source rocks were also in proximity to supply oil and gas to these reservoir rocks. Most limestone strata do not have a matrix that makes them permeable enough for oil and gas to migrate through them. However, many limestone reservoirs contain fracture systems and/or interconnecting vugs (cavities formed when acidic water dissolved some of the carbonate). These fractures and vugs, created after deposition, provide the porosity and permeability essential for oil to migrate and be trapped. Another carbonate rock, dolomite, exhibits matrix permeability mat allows fluid migration and entrapment. Dolomites also can have fracture and vugular porosity, making dolomite structures attractive candidates for oil deposits.

Salt domes. A significant portion of oil and gas production is associated with salt domes which are predominately classified as piercement-type salt intrusions and often mushroom shaped. Piercement-type domes were formed by the plastic movement of salt rising upward through more dense sediments by buoyant forces resulting from me difference in density.

Notes to the text:

1. Sedimentary гоcк - осадочная порода

2. Layer rock - слоевая горная порода

3. Silt - алеврит

4. Sand from rivers - песок из рек

5. Sandstone - песчаник

6. Permeable - проницаемый, пропускающий

7. Squeezed from the source - выжатый от источника

8. Connate water - реликтовые воды

9. To as a trap - в качестве капкана

10. Calcium carbonate - кальций карбонат

11. Calcium magnesium carbonate - кальций магниевый карбонат

12. Salt dome - соляной купол

13. Pier cement-type- цементная дамба

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