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. 但鹽岩的流動特性造成鹽岩體有多種賦存狀態，它們的地震反射特徵各不相同，這是鹽岩解釋的主要困難。
The boundary between halite and areno-argillaceous rocks show distinct reflection features because there is a strong impedance difference between them. 鹽岩與砂泥岩體之間有較強的波阻抗差，因而其界面反射特徵明顯。
