歧口凹陷凹槽区利用地震地层学解释技术研究砂体分布。
The distribution of sands in the trough zone of the depression is studied by using seismic stratigraphic interpretation method.
传统的层序地层学解释方法只是仅仅使用了常规的地震剖面和测井曲线。
Conventional sequence stratigraphy interpreting methods are only using convention seismic and well -logging data.
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