seismic basics Flashcards

(20 cards)

1
Q

What is the velocity and density of water?

A

1500 m/s
1000 kg/m^3

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2
Q

what is the equation for twt?

A

t= 2h/V

h = distnace
v = velocity

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3
Q

What is the reflective amplitude at normal incidence given by?

A

R = reflection coefficient

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4
Q

what are the equations for reflection coeffiecnt?

A

R = (DbVb – DaVa ) / (DbVb + DaVa )
or
R = (Zb-Za)/(Zb+Za)

a = above
b = below
Z = acoustic impedance

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5
Q

What is the refleciton coefficient?

A

the amplitude of the reflected wave

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6
Q

What is a seg polarity wavelet?

A

left is positve
right is negative

colour in right side

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7
Q

Why might mean Zb is bigger than Za?

A

when density or velocity is greater above then below

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8
Q

WHat happens to relfections from depth?

A

get weaker and weaker

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9
Q

What is attenuation?

A

loss of amplitude due to friction

when frequency higher wave bouncing more thus losing more energy

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10
Q

How is the dominant period defined and how can yu get frequecny from this?

A

T - distance between adjacent peaks
Frequency is inverse of T
T = 1/f

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11
Q

WHat is the limit of vertical resolution?

A

Limit of this “vertical resolution” is λ/4 (quarter wavelength) λ/4 = V / (4f)

Cannot seismically separate layers closer than this

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12
Q

What happens to frequency and velocity with depth?

A

Frequency decreases
Velocity increases

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13
Q

WHat will layers be shown as for siesmic reflection in sedimentary rocks?

A

Instead of facie chnages it will be bedding

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14
Q

What are the types of unconformity?

A

Upper boundary =Erosional truncation, Toplap, Concordance
Lower boundary = onlap, downlap, concordance

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15
Q

What will faults and strata look like in relfections?

A

Bedding planes but because of the limits of resolution we do not see all. Instead we primarily see the overall pattern of bedding: time-lines
Faults – can see where the strata are terminated against a sharp boundary

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16
Q

How does pore fill affect relfections?

A

increasing seismic velocity and density from air and gas to solid hydrates

17
Q

What is BSR?

A

Bottom simulaintg reflector = Seismic reflection event that mimics the seafloor topography and is primarily used to indicate the presence of gas hydrates beneath the seabed

18
Q

What will the polarity be when going from a denser material with higher velocity to less dense and lower velocity water?

19
Q

What will the polarity of this be BSR reflection from boundary between hydrate filled sediment (high velocity and density) and gas/water filled sediment (lower velocity and density)?