lecture 3 Flashcards

1
Q

any sedi rock can be a source rock if….

A

buried deep enough, proper temps, proper pressure, thermally mature, succient organic matter

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2
Q

what are clints

A

part of coal surface where gas is aborbed along fractures

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3
Q

what is kerogen

A

the solid and insoluable organic constituents of sedi rocks

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4
Q

what are the three stages of the hydrocarbon maturity process

A

diagenisis, catagenisis, metagensis

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5
Q

what is diagenisis

A

the initial stages of alteration of sedi rocks and maturation of kerogen

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6
Q

what is catagenisis?

A

the physical and chemical alternation of sedi and pore fluids

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7
Q

what is metagensis

A

the last stage of maturation and conversion of organic matter to hydrocarbons

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8
Q

what is biogenic and microbrial gas?

A

gas (almost pure methane) generated near the surface

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9
Q

where is the oil window

A

7000 - 18000 ft (2300 - 5500 m)

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10
Q

what is the oil temp window?

A

150 - 300 degF (65 - 150 C)

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11
Q

what is themogenic gas?

A

gas generated at depths greater than 18000 ft and 300 degF, crude turns to graphite

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12
Q

what is vitrinite reflectance

A

a measure of thermal maturity of organic matter in sedi rock

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13
Q

what are causes of HC migration

A

overburden pressure, volume increase due to maturation. capillary imibition, diffusion, buoyancy

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14
Q

formation of a trap must be ______ migration occures

A

before

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15
Q

what are the three types of petroleum reservoirs

A

limestone, sandstone, dolomite

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16
Q

name two types of carbonate reservoir rock types

A

limestone, dolomite

17
Q

name the different types of sandstones

A

aleolian, shoreline, fluvial (or alluvial), deltaic

18
Q

reefs have the most….

A

original pore space, highest recovery among carbonates

19
Q

what is oolite

A

a type of limstone made up of ooids

20
Q

what is karst limestone

A

a highly dissolved limestone

21
Q

what is dolomite

A

limestone with calcium replaced by magnesium