A mixture of different types of hydrocarbons
(fossil fuels) derived from the decomposed remains of plants
and animals that are trapped in sediment and can be used as
fuel. The petroleum group of hydrocarbons includes oil, natural
gas, and gas condensate. When plants and animals are
alive, they absorb energy from the Sun (directly through photosynthesis
in plants, and indirectly through consumption in
animals) to make complex organic molecules. After these
plants and other organisms die, they may decay to produce
hydrocarbons and other fossil fuels if the plant remains are
buried before they completely decay.
Crude oil and natural gas may become concentrated in
some regions and become mineable for use under some special
conditions. First, for oil and gas to form, more organic
matter must be produced than is destroyed by scavengers and
organic decay, conditions that are met in relatively few
places. One of the best places for oil and gas to form is on
offshore continental shelves, passive margins, or carbonate
platforms, where organic productivity is high, and the oxygen
contents of bottom waters is low so organic decay is low and
inadequate to destroy the amount of organic material produced.
Organic material may also be buried before it decays
in sufficient quantities to make petroleum in some deltaic and
continental rise environments.
Once the organic material is buried it must reach a narrow
window of specific pressure and temperature conditions
to make petroleum. If these temperatures and pressures are
not met, or are exceeded, petroleum will not form or will be
destroyed. When organic rich rocks are in this petroleum
window of specific temperature and pressure, organic rich
beds known as source rocks become compacted and the
organic material undergoes chemical reactions to form hydrocarbons
including oil and gas. These fluids and gases have a
lower density than surrounding rocks and a lower density
than water, so they tend to migrate upward until they escape
at the surface, or are trapped between impermeable layers
where they may form a petroleum reservoir.
Oil traps are of many varieties, divided into mainly
structural and stratigraphic types. Structural traps include
anticlines, where the beds of rocks are folded into an upward
arching dome. In these types of traps, petroleum in a permeable
layer that is confined between impermeable layers (such
as a sandstone bed between shale layers) may migrate up to
the top of the anticlinal dome, where it becomes trapped. If a
fault cuts across beds, it may form a barrier or it may act as a
conduit for oil to escape along, depending on the physical
properties of the rock in the fault zone. In many cases faults
juxtapose an oil-bearing permeable unit against an impermeable
horizon, forming a structural trap. Salt domes in many
places form diapirs that pierce through oil-bearing stratigraphic
horizons. They typically cause an upwarping of the
rock beds around the dome, forming a sort of anticlinal trap
that in many regions has yielded large volumes of petroleum.
Stratigraphic traps are found mainly where two impermeable
layers such as shales are found above and below a lensshaped
sandstone unit that pinches out laterally, forming a
wedge-shaped trap. These conditions are commonly met
along passive margins, where transgressions and regressions
of the sea cause sand and mud facies to migrate laterally.
When combined with continuous subsidence, passive margin
sequences typically develop many sandstone wedges caught
between shale layers. River systems and sandstone channels
in muddy overbank delta deposits also form good trap and
reservoir systems, since the porous sandstone channels are
trapped between impermeable shales.
Most of the world’s industrialized nations get the majority
of their energy needs from petroleum and other fossil fuels,
so exploration for and exploitation of petroleum is a major
national and industrial endeavor. Huge resources are spent in
petroleum exploration, and thousands of geologists are
employed in the oil industry. In the early days of exploration
the oil industry gained a reputation of being environmentally
degrading, but increased regulations and awareness by these
companies has greatly alleviated these problems, and most
petroleum is now explored for and extracted with minimal
environmental consequences. The burning of fossil fuels,
however, continues to release huge amounts of carbon dioxide
and other chemicals into the atmosphere, contributing to
global warming.
See also HYDROCARBON; PASSIVE MARGIN.














Tidak ada komentar:
Posting Komentar
Catatan: Hanya anggota dari blog ini yang dapat mengirim komentar.