Lecture 1 - Source rocks Flashcards

1
Q

What is a source rock?

A

A sedimentary rock with sufficient organic material that, when buried and heated, will produce/yield petroleum (e.g. oil and/or gas)

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2
Q

What environment do source rocks require? Give examples

A

Requires high organic productivity and stagnant water

E.g. swamps, shallow seas, lakes

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3
Q

What is required for the preservation of source rocks?

A

Low or zero oxygen contents

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4
Q

What kind of material is required for oil producing rocks? Why?

A

Organic material rich in soft, waxy tissues (e.g. algae)

Proteins, carbohydrates, lipids and lignin are required for hydrocarbon generation

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5
Q

What kind of tissue is required for generating gas source rocks?

A

Woody tissue

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6
Q

What kind of environment is required for source rocks in the sea/lakes? Give examples

A

High productivity and oxygen deficiency in water column and sea/lake bed

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7
Q

Why do lakes and seas have anoxic bottom waters?

A

Lack of circulation allowing organic material to be preserved

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8
Q

What is bitumen?

A

Compounds soluble in organic solvents

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9
Q

What are kerogens?

A

Abundant Insoluble CHO complex compounds

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10
Q

Name the four types of kerogens and briefly describe them in terms of yield, source, what they produce and fluoresces

A

Liptinite (Type 1): high yield, algal source, produces oil, fluoresces under UV
Exinite (Type 2): lower yield (40-60%), plant source, produces oil, fluoresces under UV
Vitrinite (Type 3): low yield, plant source, produces gas, does not fluoresces under UV
Inertinite (Type 4): High C, low H, ‘dead’ carbon

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11
Q

When are large molecules of kerosene stable?

A

Low temperatures

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12
Q

What happens with progressive heating of kerosene? What is released?

A

Breaks down to smaller molecules of liquid and gaseous hydrocarbons. CO2, H20 and residues released

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13
Q

What is the oil window? (temps and depth)

A

60-120 degrees C

2-4km depth

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14
Q

What is the gas window?

A

100-200+ degrees C

2-6km

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15
Q

What is the most important control for hydrocarbon maturation?

A

Temperature

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16
Q

Where does heat come from at depth?

A

Basement (radioactive decay) and residual mantle heat

17
Q

What is the typical temp/depth gradient? Give examples of a cool and hot basin

A
Typical gradient is 20-40 degrees C/km
Cool basins (e.g. Caspian Sea), 50 C/km
18
Q

What are the primary products of maturation

A

CO2 and H2O

19
Q

What causes tar mats to form?

A
late influx of gas into an oil filled reservoir => due to decreased solubility of heavy compounds
Thermal cracking (elevated Ts)
20
Q

What influences maturation in reservoir?

A

Further influence of temperature