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Chapter 2 – OIL AND GAS RESERVOIR FORMATION 25
very close to each other. At a depth of 2,000 m, the gap between the
crystals is about 10 nanometers. By the time the shale is buried to a depth
of 5,000 m, this gap has closed to about 1.5 nanometers (1.5 × 10 m or
–9
0.0000000015 m).
Shale has tiny pores that are connected by tiny passages. It takes a long
time for the water and the oil produced within the shale source rock to
migrate out of the rock, squeezed out by pressure. The actual mechanism
by which the oil leaves the source rock is uncertain, but it is thought that
the oil is initially in solution in the water under the high pressures that exist
in the source rock.
Primary Migration
The first two conditions necessary for the birth of a reservoir are the
existence of an organic-rich source rock and the conditions necessary for
oil to be generated—temperature (the oil window) and time. If the oil
cannot migrate out of the source rock, it stays locked within the shale and
cannot be produced.
The third element required is that the source rock lies next to a
permeable rock or a channel that allows the oil to migrate. In most cases,
a permeable sandstone deposit provides this conduit, but it can also be
provided by fractures in the rock or ancient reefs (limestone structures
made up of coral skeletons with very high permeability). Fractures often
allow migration vertically upwards, and this mechanism has led to many
large oil accumulations, such as those found at shallow depths in Venezuela
and northern Iraq.
A gently sloping formation bed can carry the oil for long distances
horizontally until a trap stops migration and allows accumulation.
Therefore, a reservoir can be located many miles away from the source
rock that generated the oil.
Structural Traps
As the oil and gas undergoes primary migration away from the source
rock, it must find a structure that has the right conditions to trap the oil and
stop it from reaching the surface (fig. 2–2).
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