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Question

Given the statements, I and II, which one of the following options is correct?
Statement I: ScP and PcS phases of a near-surface earthquake arrive at an observatory at different times
Statement II: ScP phase of a deep focus earthquake arrives earlier than PcS phase at the same observatory

The correct answer is
Statement I is false but statement II is true

Seismic Wave Arrival Time Analysis: Statements I & II

Statement I: Near-Surface Earthquake Phases

Statement I: ScP and PcS phases of a near-surface earthquake arrive at an observatory at different times.

Assessment: False.

  • ScP (S-wave converts to P-wave at the Core-Mantle Boundary, CMB) and PcS (P-wave converts to S-wave at the CMB) involve distinct paths.
  • For near-surface earthquakes, path lengths are relatively short. The arrival time calculation involves travel from the source to the CMB and then from the CMB to the station.
  • Let $T_{S \to CMB}$ and $T_{P \to CMB}$ be the travel times of S and P waves from the source to the CMB, respectively. Let $T_{P \to Sta}$ and $T_{S \to Sta}$ be the travel times of P and S waves from the CMB to the station.
  • The arrival time for ScP is $T_{ScP} = T_{S \to CMB} + T_{P \to Sta}$.
  • The arrival time for PcS is $T_{PcS} = T_{P \to CMB} + T_{S \to Sta}$.
  • Although $T_{S \to CMB} > T_{P \to CMB}$ (since S-wave speed is slower than P-wave speed in the mantle) and $T_{P \to Sta} < T_{S \to Sta}$ (since $v_p > v_s$ in the mantle), the specific path lengths for near-surface sources can cause $T_{ScP}$ to be very close to $T_{PcS}$.
  • Therefore, their arrival times are often practically indistinguishable, making the statement that they arrive at definitively different times false in an observational context.

Statement II: Deep Focus Earthquake Phases

Statement II: ScP phase of a deep focus earthquake arrives earlier than PcS phase at the same observatory.

Assessment: True.

  • Deep focus earthquakes originate deep within the Earth.
  • Both ScP and PcS phases involve travel from the CMB to the seismic observatory.
  • The ScP phase travels this final segment as a P-wave.
  • The PcS phase travels this final segment as an S-wave.
  • In the Earth's mantle, P-wave velocity ($v_p$) is greater than S-wave velocity ($v_s$), i.e., $v_p > v_s$.
  • Consequently, the travel time for the P-wave segment from the CMB to the station ($T_{P \to Sta}$) is shorter than the travel time for the S-wave segment ($T_{S \to Sta}$) over the same distance.
  • This ensures that the ScP phase arrives earlier than the PcS phase.

Conclusion on Statements

Statement I is false, and Statement II is true. This corresponds to Option D.

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Important Questions from Seismology

  1. A geophysicist travelling from the Bay of Bengal through the Ganga plain to the Himalaya, estimates the depth of Moho discontinuity. Which one of the following is the correct order of the Moho-depth estimates?
  2. Compressional wave velocity is the highest in
  3. If $V_m$, $V_o$ and $V_i$ are the average P-wave velocities in the lower mantle, outer core and inner core respectively, then
  4. PKS and SKP phases of a surface focus earthquake reach an observatory
  5. In a homogeneous isotropic medium with a free surface
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