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一、前言地下卤水矿床的形成理论,早已引起中外地质学者注视。四川邓井关背斜三迭系黑卤水先后有省石油、地质等部门对本地区的地层、构造气、卤储集的一般规律作了不同程度的探查研究工作,为探讨黑卤水矿床的形成提供了宝贵资料。作者认为,邓井关背斜三迭系(T_1j~5+T_2L~1)黑卤水矿床的形成,绝非单一因素,
I. Preface The formation theory of underground brine deposits has long attracted the attention of Chinese and foreign geologists. The tributary black brine of the Dengjingguan anticline in Sichuan Province has made some exploration and research work on the general laws of strata, structural gas and brine reserves in the provinces and regions such as the petroleum and geology departments, so as to provide a probe into the formation of black brine deposits The valuable information. The author believes that the formation of the Tangjingguan anticline Triassic (T_1j ~ 5 + T_2L ~ 1) black brine deposits is by no means a single factor,