Summary
Highlights
Despite oil extraction plants often being on land, all oil deposits originated in the sea millions of years ago. Fine marine sediments are crucial for the formation of hydrocarbon deposits.
When marine microorganisms die, their remains settle on the seabed, and the organic matter is covered by sediments. This forms a dark mud called sapropel, rich in organic matter. Further sedimentation prevents oxidation and decomposition, transforming the sapropel into source rock, still rich in organic material.
Over millions of years, increased pressure and temperature from overlying sedimentary layers transform the trapped organic matter in the source rock into hydrocarbons, specifically oil and gas. The pressure from these gases and Earth's crustal movements compress the source rock, expelling the hydrocarbons.
These hydrocarbons then migrate from the source rock to overlying reservoir rock, typically porous and permeable sandstone capable of holding the hydrocarbons in its interstices. To prevent dispersion, an impermeable rock layer must be present above the reservoir rock.
If crustal movements create an anticline (a dome-shaped fold), the impermeable rock becomes an effective trap for the hydrocarbons, creating a perfect condition for an oil deposit. Within the reservoir rock, water, oil, and gas distribute themselves according to density: gas at the top, then oil, and water at the bottom. This allows for the construction of a well to exploit the deposit.