Lecture 4 Flashcards

Seismic Methods

1
Q

What are the main applications of seismic methods

A
  • hydrocarbon exploration
  • mineral exploration
  • research into Earth’s structure
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2
Q

What are the seismic reflection and refraction methods

A

Measuring the time taken for a seismic wave to travel from a source, down into the ground where it gets reflected/refracted back to the surface where it is recorded.

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3
Q

What do ‘travel-times’ allow to be calculated

A

Allow wave velocities to be calculated and wave paths to be inferred

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4
Q

What is snells law?

A

sini/sinr = v1/v2

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5
Q

What is the angle of incidence equal to?

A

Angle of refraction

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6
Q

What does reflection depend on?

A

Acoustic impedence

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7
Q

Why can surface waves complicate seismic surveys?

A

As they are also recorded by geophones on the Earth’s surface

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8
Q

Define critical refraction

A

When V2>V1, there will be an incident angle for which the refracted angle is 90 degrees.

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9
Q

Define Acoustic impedence contrast

A

Contract between layers determines the amplitude pf reflected seismic phases

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10
Q

What is acoustic impedence the property of?

A

Density and velocity

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11
Q

If acoustic impedence = 0, will refraction

A

Refraction can still occur.

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12
Q

If Z1 and Z2 are the same, reflection can occur. True or False

A

False. Reflection will not occur.

All energy will be transmitted along the interface.

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13
Q

What are seismic refraction surveys designed to do?

A

Acquire information about the subsurface from seismic waves that are refracted and post-critically refracted. When incident upon a boundary where there is a constant velocity.

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14
Q

What are seismic reflection surveys designed to do?

A

Acquire information about the subsurface from seismic waves that are critically reflected when there is no acoustic impedance contract.

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15
Q

wave fronts that propagate back to the surface are called what?

A

Head waves

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16
Q

The relative proportions of the seismic wave energy that are reflected and transmitted are known as what?

A

Zoepritt’s equations

17
Q

Define Zoepritts equations

A

The relative proportions of the seismic wave energy that are reflected and transmitted

18
Q

What can zoepritts equations be written in terms as?

A

Can be written in terms of the acoustic impedance of the two layers

19
Q

Define the reflection coefficient

A

The reflection coefficient is the ratio of the reflected ray (A1) to the amplitude of the reflected ray (A0)

20
Q

Define propagation velocity

A

The velocity with which the seismic energy travels through a medium

21
Q

is the reflected phase the first to arrive?

A

No, it never is, it comes sooner once it is beyond the critical distance

22
Q

Define crossover distance

A

The offset at which the arrival times of critically refracted waves preceded those of the direct waves

23
Q

Define critical distance

A

At the critical distance the reflected arrival is coincident with the first critically refracted arrival, the travel times of the two are identical.