• Title/Summary/Keyword: 이동식 진동기

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Analysis of source characteristics for high-resolution seismic surveys on a tidal flat (조간대 지역에서의 고해상 탄성파 탐사를 위한 파원 특성 분석)

  • Hong, Jong Guk;Kim, Gi Yeong;Kim, Han Jun
    • Journal of the Korean Geophysical Society
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    • v.2 no.2
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    • pp.100-110
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    • 1999
  • In order to find a good seismic source for high-resolution reflection surveys on a tidal flat, characteristic features of several sources were examined through test recording by the walkaway configuration. The sources comprise portable vibrator, 1.2 kg monkey spanner, 4.7 kg sledge hammer, and weight drops with a 30 kg and a 100 kg iron ball, respectively. We analyzed raw and filtered seismic data for the resolution of individual events, then compared various seismic sources to define suitable one for the high-resolution survey in terms of energy level and frequency contents. The study reveals that the portable vibrator is the most suitable source for the detection of and imaging geologic structures less than 20-30 m deep in a tidal flat. We ascribe this to the wide frequency band and high-frequency contents of the portable vibrator. In contrast, the hammer may be an alternative where the target depth increases up to 100 m.

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A High-resolution Seismic Survey on the Abandoned Tidal Flat in Shihwa Lake (시화호내 과거 조간대에서의 고해상 탄성파 탐사)

  • Hong, Jong Guk;Kim, Gi Yeong;Choe, Dong Rim
    • Journal of the Korean Geophysical Society
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    • v.2 no.4
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    • pp.251-258
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    • 1999
  • A high-resolution seismic survey was conducted on the abandoned tidal flat in Shihwa Lake on the west coast of Korea. A portable vibrator was used as a seismic source and 217 shot gathers with 48-channel system were acquired. F-k filtering, residual static corrections and post-stack frequency filtering are found to be useful for signal enhancement. The overburden is divided into two seismic depositional units. Unit I is deposited in tidal environment characterized by parallel and high continuity reflection pattern. This unit comprises a dry layer (Unit Ia) and a wet layer (Unit Ib) having averagely 5 and 15 meters thick, respectively. Unit II unconformably overlain by Unit I exhibits discontinuity and hummocky reflection pattern, indicating complex channel-fill sediments in estuary. The maximum thickness of this unit is approximately 20 meter. Acoustic basement is considered as Precambrian granitic gneiss occurred in the surrounding area.

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