Seismic Refraction Flashcards

1
Q

What are the 2 types of applied seismology?

A
  1. Seismic refraction
  2. Seismic reflection
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2
Q

What is seismic refraction

A

Signal returns to surface by refraction and recorded at a distance greater than depth

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3
Q

What is seismic reflection?

A

Seismic signal reflected back to surface and recorded at distances less than depth

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4
Q

What are the 2 types of strain that can propagate as waves?

A
  1. Axial streas
  2. Shear stress
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5
Q

What is hookes law?

A

Stress is proportional to strain

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6
Q

What are the 2 types of body waves?

A

1.P-waves
2. S-waves

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7
Q

What are P-waves?

A

Where the motion of particles in a solid is the direction of wave propagation (horizontal vibrations). HIGHEST speed

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8
Q

What are S-waves? Why can’t S-waves exist in fluids like water or air?

A

Particle motion is in plane perpendicular to direction of propagation (vertical vibrations) with no volume change.

Because the fluid is unable to support shear stresses.

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9
Q

What are the 2 types of surface waves?

A
  1. Rayleigh waves
  2. Love waves
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10
Q

What are Rayleigh waves? What happens to the amplitude with depth?

A

Waves that propagate along the surface of the Earth.

Amplitude decreases a lot with depth

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11
Q

What are love waves? How do they propagate? When do they occur?

A

Waves that move horizontally and vibrate perpendicular to propagating.

Occur when free surface and deeper interface are present and the shear wave velocity is lower in the top layer

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12
Q

What do seismic wave velocities depend on (3)?

A

Density
Shear modulus
Axial modulus

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13
Q

In igneous rocks, how does velocity increase?

A

With increase in mafic content

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14
Q

If there is an increase in porosity, how does that affect the seismic velocity?

A

Decrease in seismic velocity with increase in porosity

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