Chapter 1 - Origins of Oil & Gas Flashcards
For hydrocarbons to accumulate, three conditions must be met, what’s first?
First, a sedimentary basin must be created-the result of movement of the earth’s crust, which creates large depressions into which sediments from surrounding elevated areas are transported over time.
For hydrocarbons to accumulate, three conditions must be met, what’s second?
Second, the sediments laid down in such basins must contain a high level of organic material. This organic-rich matter becomes part of the sedimentary material to create what is called source rock.
For hydrocarbons to accumulate, three conditions must be met, what’s third?
Third, over millions of years, the effects of elevated temperature and pressure must be sufficient to convert the material in the source rock into oil and gas.
Define maturity.
Maturity describes the degree to which petroleum generation has occurred. Heavy, thick oil is considered immature, having been generated at relatively low temperature. Mature oil – lighter or less viscous – forms at higher temperature.
Define migration.
In an important subsequent process called migration, the hydrocarbons must move out of the source rock through cracks, faults, and fissures and into porous and permeable reservoir rock.
Petroleum geochemists and geologists widely agree that crude oil is derived what?
Ancient organic matter-ranging from single-celled plankton to more-complex aquatic plants (e.g., algae) and even invertebrates and fish-laid down and then buried and preserved in sediments eons ago at the bottom of ancient oceans.
Define kerogen.
As the sediment layer gets thicker, subsequent bacterial processes at work in deep seabed mud (with little or no oxygen present in the mud itself or the water immediately above it) convert the remaining organic matter into a waxy material called kerogen.
What is the composition of kerogen?
Kerogen is a complex mixture of large organic molecules whose appearance and characteristics depend on the kind and concentration of materials—such as algae, plankton, bacteria, pollen, resin, and cellulose— of which it is composed. It is from kerogen that oil and gas are generated.
Organic matter was not laid down evenly through the various geologic eras (table 1–1). Accumulations were clearly concentrated in a limited number of intervals whose duration was determined by movements in the earth’s crust and by climatic changes. Different periods contributed the following approximate shares of the world’s kerogens:
Middle Cretaceous (about 100 million years ago): nearly 30% Late Jurassic (150 million years ago): 25% Late Devonian (350 million years ago): less than 10% Silurian (420 million years ago):less than 10% Early Cambrian (550 million years ago): less than 10%
The total amount of organic matter stored in the earth’s crust has been estimated to be what?
10 quadrillion (1016) tons, of which approximately 1% (100 trillion [1014] tons) is in organic-rich rocks—principally, shales containing at least 3% organic matter.
Kerogen concentrations as low as ____ are generally sufficient to be make source rock (typically shales and limestones) suitable for commercial exploitation of crude oil and natural gas.
1%–3%
What is the most common kind of source rock?
Black Shale
Define Thermal Gradient.
Temperature plays a key role in the generation of oil and gas from kerogen. As the organic-rich source rock undergoes progressive burial (i.e., as additional sediments are laid down above it), the rock becomes hotter.This phenomenon reflects what is called the geothermal gradient of the earth.
For tectonically stable shield areas and sedimentary basins, what is the typical ratio?
1.5-2C per 30.5 meters
Define Oil Window.
Oil Window is used to describe the range of temperature or depth within which most of oil’s complex constituents are produced (fig. 1–1).This window is typically 80–220°C (176–428°F) or 2,200– 5,500 meters (7,200–18,000 feet).
Did you describe it well?
At what temperatures does kerogen being to be transformed into oil?
Below a temperature of about 50°C (122°F), small amounts of kerogen begin to be transformed into oil. Peak conversion occurs at about 100°C (212°F).