The paper argues that the salt rocks are deposited in shallow water, the salt comes from the Lower-Middle Ordovician series of the surrounding uplifts.

 
  • 這一認識不同于過(guò)去“高山深盆”、“深水成鹽”和“海相成因”的觀(guān)點(diǎn),將給東濮凹陷沉積古地理、古環(huán)境研究帶來(lái)新的認識。
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