世界上大多数含盐盆地都是含油气区。
The majority of salt-bearing basins in the world are petroliferous basin.
主要的地表铜矿物是氯铜矿，为干旱气候条件下含盐盆地的产物。
The main copper mineral is atacamite on the surface, which form on droughty climate conditions in salt basin.
在许多沉积盆地中，地层水的含盐量随深度或压实作用而增高。
In many sedimentary basins the salinity of the formation water increases with depth or compaction.
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