Isochronal horizons can be obtained through recognizing types of seismic unconformity boundary, the features of seismic facies and the relations of sandbody overlapping.

 
  • 根據地震不整一邊界類(lèi)型、地震相特征、砂體疊置關(guān)系變化可以確定小層等時(shí)界面,并且等時(shí)界面可以從波峰等時(shí)漸變到波谷;
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