However, due to the flow feature, halite has several modes of occurrence and their seismic reflection features are different, which makes it difficult to recognize halite. 但鹽巖的流動(dòng)特性造成鹽巖體有多種賦存狀態(tài)，它們的地震反射特征各不相同，這是鹽巖解釋的主要困難。
The boundary between halite and areno-argillaceous rocks show distinct reflection features because there is a strong impedance difference between them. 鹽巖與砂泥巖體之間有較強的波阻抗差，因而其界面反射特征明顯。
