In the upper Jurassic to Tertiary, there is the alkali diagenetic ambient, in which the inter-pore fluid is inherited from the buried syngenetic water, i.e.

 
  • 上侏羅紀至第三系為堿性成巖環(huán)境,隙間流體繼承了封存同生水特征,為堿性鹽鹵水。
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