hydrocarbon traps & seals
DESCRIPTION
Hydrocarbon Traps & SealsTRANSCRIPT
Hydrocarbon Traps and Seals
Revision
What are geological elements of petroleum system?
What are geological processes of petroleum system?
How organic matters is converted into petroleum?
• Source Rock - A rock with abundant hydrocarbon-prone organic matter
• Reservoir Rock - A rock in which oil and gas accumulates:
- Porosity - space between rock grains in which oil accumulates
- Permeability - passage-ways between pores through which oil and gas moves
• Seal Rock - A rock through which oil and gas cannot move effectively (such as mudstone and claystone)
• Migration Route - Avenues in rock through which oil and gas moves from source rock to trap
• Trap - The structural and stratigraphic configuration that focuses oil and gas into an accumulation
Top of oil window
Top of gas window
Generation Expulsion Accumulation
GOC
OWC
Migration Preservation
The processes
(modified from Tissot and Welte, 1984)
Organic Debris
Kerogen
Carbon
Initial Bitumen
Oil and Gas
Methane
Oil Reservoir
MigrationThermal Degradation
Cracking
Diagenesis
Catagenesis
Metagenesis
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gSchematic Representation of the Mechanism
of Petroleum Generation and Destruction
i. Diagenesis is chemical, physical, or biological change undergone by a sediment after its initial deposition and during and after its lithification, exclusive of surface alteration (weathering) and metamorphism. These changes happen at relatively low temperatures and pressures and result in changes to the rock's original mineralogy and texture. There is no sharp boundary between diagenesis and metamorphism, but the latter occurs at higher temperature and pressure than the former. ii. Catagenesis Catagenesis is the cracking process which results in the conversion of organic kerogens into hydrocarbons
iii. Metagenesis is the last stage of maturation and conversion of organic matter to hydrocarbons. Metagenesis occurs at temperatures of 150° to 200°C. At the end of metagenesis, methane, or dry gas, is evolved along with nonhydrocarbon gases such as CO2, N2, and H2S, as oil molecules are cracked into smaller gas molecules.
What is TrapA trap is the place where oil and gas are barred
from further movement….(Levorsen, 1967)
.
Seals or Cap RocksFor a trap to have integrity, it must be overlain
by an effective seal.Any rock that is impermeable can act as seal or
cap rock but commonly mudstone
Introduction: Oil Traps• Some rocks are permeable and allow oil and gas to freely pass through them
• Other rocks are impermeable and block the upward passage of oil and gas
• Where oil and gas rises up and capped by impermeable rocks it can’t escape. This is one type of an Oil Trap.
Impermeable
Permeable
• The permeable rocks than contain oil and gas within the oil trap are known as the Reservoir Rock.
• Reservoir rocks have lots of interconnected holes called pores. These allow them to absorb the oil and gas like a sponge.
Earth Science World Image Bank Image #h5innl
This is a highly magnified picture of a sandy reservoir rock (water-filled pores are shown in blue)
As oil migrates it fills up the pores(oil-filled pores shown in black)
Carbonate as Reservoir
How to find oil: Source rock, reservoir rock, traps
Hydrocarbon Trapsi. Structural traps
Structural traps are caused by structural features. They are usually formed as a result of tectonics.
ii. Stratigraphic traps
Stratigraphic traps are usually caused by changes in rock quality.
iii. Combination traps
Combination traps that combine more than one type of trap are common in petroleum reservoirs.
Other types of traps (such as hydrodynamic traps) are usually less common.
Structural Hydrocarbon Trapsi. Fold ii. Fault
iii. Salt Dome
Salt flows up as a weak mass
Petroleum trapped in top of dome
Oil and gas trapped on sides of impermeable dome
Rocks above salt dome are bowed up
iii. Salt Dome
Fault Trap
Oil / GasSand
Shale
In this normal fault trap, oil-bearing sandstone is juxtaposed against impervious shale.
Stratigraphic Hydrocarbon Traps
(modified from Bjorlykke, 1989)
Stratigraphic hydrocarbon traps occur where reservoir facies pinch into impervious rock such as shale, or where they have been truncated by erosion and capped by impervious layers above an unconformity.
Asphalt Trap
Hydrodynamic Trap
Water
MeteoricWater
BiodegradedOil/Asphalt
PartlyBiodegraded Oil
Shale
OilWater
HydrostaticHead
(modified from Bjorlykke, 1989)
Other Traps In hydrodynamic traps, the hydrocarbon is trapped by the action of water movements. Tilted contacts are common in this case. The water usually comes from a source such as rain falls or rivers.
Summary
Questions?