Module 10a- Reservoir Geology Flashcards

1
Q

What are the 4 types of porosity

A

Intergranular
Inter- & Intragranular
Moldic porosity
Vuggy porosity

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2
Q

What are the 2 types of diagentic porosity loss mechanisms?

A
Mechanical (compaction, plastic deformation, brittle deformation, fracturing)
and Chemical (precipitation, dissolution)
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3
Q

What does diagentic porosity loss result from?

A

compaction and cementation

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4
Q

What is the dominant process when in the early stages of diagenesis?

A

Compaction

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5
Q

What does compaction cause?

A

deformation of the grains

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6
Q

Deformation can be either?

A

brittle or plastic depending on the lithology and mineralogy of the grains

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7
Q

What occurs from deformation?

A

grains get further compacted, thus reducing porosity

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8
Q

What is compaction?

A

is the dominant process when in the early stages of diagenesis grains and re-arranged and fluids are expelled from the shrinking pores.

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9
Q

Where does maximum reduction occur in compaction?

A

in muddy sediments containing large amount of fluids. Also, carbonated grainstones also get compacted.

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10
Q

What occurs when the fluid is expelled during compaction?

A

Can cause chemical porosity enhancement of reduction due to a number of diagenetic reactions.

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11
Q

What occurs when the cements and the original grains are comprised of the same mineral?

A

porosity loss

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12
Q

What 2 kinds or rocks does porosity enhancement occur in?

A

siliclastic and carbonate

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13
Q

What is the most common porosity enhancement seen in?

A

carbonates as the carbonate rocks dissolves more easilt than quartz

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14
Q

How can porosity be enhanced in siliclastic rocks?

A

Dissolution of cements

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15
Q

What are the main factors controlling mineral precipitation between grains (cementation)?

A

Chemistry of the sediment
Composition/concentration of pore fluid
Temperature

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16
Q

What are the most common reservoir rocks?

A

Siliciclastics and carbonates

17
Q

Mineral cements are most commonly composed of what?

A
The same minerals as the grains
example:
siliciclastic rocks, silica cement is common
and
carbonates , carbonate cement is common
18
Q

What does biogenic amorphous silica tend to dissolve in?

A
Alkaline waters (pH > 7)
Note: the process is the other way around in Carbonates
19
Q

In carbonate rocks, fragments and grains in a reef, for example, become cemented when?

A

at a very early stage - prior to a deep burial

20
Q

Carbonate cements are mainly precipitated from carbonate solutions during a ….?

A

Super-saturation stage, where the concentration of dissolved carbonate is so high that precipitation occurs

21
Q

When is a reservoir considered over pressure?

A

it is dependent on the gradient and happens when it is higher than normal (10kPa/m)

22
Q

When does over pressure mainly occur? And when is it common?

A

when there is rapid burial which does not allow sufficient time for pore fluids to escape
Common in deeply - buried sedimentary rocks (Gulf of mexico / Niger Delta)

23
Q

what causes Geological overpressure ?

A

Rapid burial of sediments along with fluids not being able to escape because they are surrounded by impermeable beds

24
Q

overpressure is also encountered where? and what are two examples?

A

In foreland basins in front of mountain ranges

ex: The rocky mountains in Alberta and N.E. BC in an area known as the Deep Basin

25
Q

Overpressure formations are usually what ?

A

Undercompacted because the pore fluid supports some of the weight of the overlying rock strata.

26
Q

How does the undercompacted property of an overpressured formation affect seismic waves?

A

slows them down and therefore overpressure can be detected on sonic logs from seismic data

27
Q

What is the most common matrix mineral found in siliciclastic petroleum reservoirs ?

A

Clay minerals

note: in carbonate reservoirs , clays are much less common

28
Q

Clays are also the most important mineral of what ?

A

Shales

29
Q

Why are clays important in the geology of petroleum?

A

because they vary in amounts and effect many problems connected with the porosity and permeability of the reservoir

30
Q

Shale makes up of approximately how much of the sedimentary rocks on record?

A

more than half , so it is basically the most common sedimentary rock there is

31
Q

What is shale composed of?

A

Different clay minerals, precipitates and very fine clastic particles.

32
Q

The most important aspect of clay minerals is what?

A

their ability to hold adsorbed water on their grain surfaces

33
Q

What three ways can shale be distributed in sand?

A

Laminated, structural and dispersed shale

34
Q

What has the greatest effect in reducing the original porosity?

A

Dispersed shale because it consists of clay overgrowths on sand grains, or accumulations which partially fill pore space.

35
Q

what does laminated shale consist of?

A

either thin shale beds or streaks, between sand beds

note: the layers have no effect on the inter-matrix porosity or perm

36
Q

what does structural shale have to do with?

A

The random placement of individual grains of the primary matrix material with fragments of lithified reworked shale

37
Q

Does structural shale replace matrix or add to it? and what is the effect on porosity?

A

it replaces the matrix and usually on a small scale sot here is very little to no effect on porosity and perm

38
Q

what constitutes dirty sand

A

sand containing a lot of clay and so therefore sand with little clay is clean sand

39
Q

which clay is detrimental to the drilling process?

A

Montmorillonite because it is susceptible to swelling when exposed to fresh water