The shallow sedimentary basin structure can be obtained from reflection seismic data;basement undulation and deep structure can be obtained from gravity and magnetic inversion.

 
  • 淺層沉積盆地結構通過(guò)反射地震資料控制,深層地質(zhì)結構信息利用重磁異常場(chǎng)分離、物性界面反演等方法得到。
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