Abstract:A potash deposit, which was discovered, for the first time, a few years ago, is located in the Dawenkou Basin of Shandong Province in Chine. The potash-bearing bed occurs as an intercalated one in the multi-beds of rock salt in the second member of the Guanzhuang formation of the Eocene-Oligocene sediments. The author has proposed some views in terms of the specific conditions of the potash salt deposition based on the geological and geophysical exploration results and synthesized relevant data:1.The salt-b...