Parameter analysis for gas hydrate data of East sea using Geobit

지오빗을 이용한 동해 가스하이드레이트 탄성파 자료처리 매개변수 분석

  • 김영완 (한국지질자원연구원 석유해저자원연구부) ;
  • 장성형 (한국지질자원연구원 석유해저자원연구부) ;
  • 김현태 (한국지질자원연구원 석유해저자원연구부) ;
  • 윤왕중 (전남대학교 지구시스템공학과)
  • Published : 2006.06.22


A seismic survey for gas hydrate have performed over the East sea by the KIGAM since 1997. General indicator of gas hydrate in seismic data is commonly inferred from the BSR(Bottom Simulating Reflector) that occurred parallel to the sea floor, amplitude decrease at the top of the BSR, amplitude blanking at the bottom of the BSR, decrease of the interval velocity and the reflection phase reversal at the BSR. In this paper we had analyzed optimum parameters of the field data to detect the 9as hydrate. Shot delay correction is applied 95ms, spherical divergence correction is applied velocity library 3, bandpass filter is applied 25-30-115-120Hz deconvolution operator length is applied 60ms, lag is 6ms and accurate velocity analysis NMO correction, stack is performed. Geobit 2.11.0 developed by the KIGAM was used for all data processing. Processing results say that the BSR occurred parallel to the sea floor were shown at 3,150m/s of two way travel time from the sea floor through shot point 5,000-5,610, and identified the interval velocity decrease around BSR and the reflection phase reversal corresponding to the reflection at the sea floor.