Petroleum, also known as crude oil, is a fossil fuel formed from the remains of ancient marine organisms. The process of its formation is complex and takes millions of years, generally summarized in these steps:
Organic Matter Deposition: Millions of years ago, microscopic marine organisms like algae and plankton thrived in shallow seas. When these organisms died, their remains settled to the ocean floor, accumulating along with other sediments like sand, silt, and clay.
Burial and Sedimentation: Over time, layers of sediment accumulated on top of the organic-rich layer, burying it deeper and deeper. The increasing weight and pressure compacted the sediment, squeezing out water and reducing the volume of the organic matter.
Anaerobic Decomposition: In the absence of oxygen (anaerobic conditions), bacteria partially decomposed the organic matter. This process produced a thick, dark, organic-rich mud called sapropel. Complete decomposition wasn't possible due to the lack of oxygen.
Diagenesis and Catagenesis: As burial continued, temperature and pressure increased significantly. This led to diagenesis, the initial phase of transformation where the sapropel was chemically altered. Further burial and increasing temperature initiated catagenesis, where kerogen, a complex mixture of organic molecules, was formed. This is a crucial stage because kerogen is the precursor to petroleum.
Oil Generation (Catagenesis): As temperature continued to rise (typically between 60-150°C), kerogen began to break down through thermal cracking, releasing hydrocarbons (molecules made of hydrogen and carbon). These hydrocarbons are the main components of petroleum—a mix of liquid (crude oil) and gaseous (natural gas) substances. The specific temperature range and pressure affect the type of hydrocarbons produced, influencing the quality of the oil (e.g., heavier or lighter crude).
Migration and Accumulation: The newly formed hydrocarbons, being less dense than water and surrounding rock, began to migrate upwards through porous and permeable rocks like sandstone. Eventually, this migration was halted by impermeable rock layers, such as shale, creating traps where the oil and gas accumulated in large reservoirs. These geological formations are crucial for economically viable oil and gas fields.
Entrapment and Reservoir Formation: The accumulated hydrocarbons in these traps form reservoirs, where they remain until discovered and extracted. The type of trap (structural or stratigraphic) and the cap rock's integrity determine the size and longevity of the reservoir.
In summary, petroleum formation is a long and complex geological process involving the burial of organic matter, transformation under heat and pressure, migration through permeable rocks, and ultimately, entrapment in underground reservoirs. The precise conditions at each stage determine the type and quantity of petroleum formed.