By using this method, it was revealed that the sandbodies distribution trend and sedimentary microfacies analysis results have high correlativity in Dongpu depression. 利用以上方法在東淮凹陷某三維地震工區進(jìn)行了儲層預測，預測的砂體分布趨勢與沉積微相的解釋結果相關(guān)程度較高，符合該區的地質(zhì)規律。
It is found that the distribution tendencies of these parameters were similar and corresponded to the geostrophic current fields. 研究結果表明，上述諸要素的分布趨勢是一致的，且與地轉流場(chǎng)相對應。
