• Title/Summary/Keyword: 가스하이드레이트, 오호츠크해, 가스기둥, 가스분출기둥, 지구물리탐사

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Geophysical Investigation of Gas Hydrate-Bearing Sediments in the Sea of Okhotsk (오호츠크해 가스하이드레이트 퇴적층의 지구물리 탐사)

  • Jin, YoungKeun;Chung, KyungHo;Kim, YeaDong
    • Journal of the Korean Geophysical Society
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    • v.7 no.3
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    • pp.207-215
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    • 2004
  • As the sea connecting with the East Sea, the Sea of Okhotsk is the most potential area of gas hydrates in the world. In other to examine geophysical structures of gas hydrate-bearing sediments in the Sea of Okhotsk, the CHAOS (hydro-Carbon Hydrate Accumulation in the Okhotsk) international research expedition was carried out in August 2003. In the expedition, high-resolution seismic and geochemical survey was also conducted. Sparker seismic profiles show only diffusive high-amplitude reflections without BSRs at BSR depth. It means that BSR appears to be completely different images on seismic profiles obtained using different frequencies. Many gas chimneys rise up from BSR depth to seafloor. The chimneys can be divided into two groups with different seismic characteristics; wipe-out (WO) and enhanced reflection (ER) chimneys. Different seismic responses in the chimneys would be caused by amount of gas and gas hydrates filling in the chimneys. In hydroacoustic data, a lot of gas flares rise up several hundreds meters from seafloor to the water column. All flares took placed at the depths within gas hydrate stability zone. It is interpreted that gas hydrate-bearing sediments with low porosity and permeability due to gas hydrate filling in the pore space make good pipe around gas chimneys in which gas is migrating up without loss of amount. Therefore, large-scale gas flare at the site on gas chimney releases into the water column.

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Geophysical investigation of methane seeps on the NE Sakhalin continental slope, Sea of Okhotsk (오호츠크해 북동사할린 대륙사면에 나타나는 메탄분출구에 대한 지구물리탐사)

  • Jin, Young-Keun;SSGH-Scientific-Party, SSGH-Scientific-Party
    • 한국지구물리탐사학회:학술대회논문집
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    • 2008.10a
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    • pp.137-140
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    • 2008
  • During CHAOS (2003, 2006) and SSGH projects (2007), acoustic investigation including hydroacoustic (HA), side-scan sonar (SSS) and highresolution sparker seismic (HSS) surveys was carried out on the northeastern Sakhalin slope ($53^{\circ}56'\;N$, $143^{\circ}52'\;E$ to $54^{\circ}40'\;N$, $144^{\circ}32'\;E$). More than 130 methane seeps with high backscatter intensity are identified on SSS mosaic, which are well accompanied with gas flares in the water column on HA profiles and subbottom gas chimneys on HSS profiles. It is likely that that some seeps align along a NW strike parallel to the Lavrentiev Fault.

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