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笔者根据一九八四年山东石臼港区供水水文地质测绘工作中地质、地貌调查资料及山东省地矿局地质二队钻孔资料,对测区的新构造运动的表现、类型、强度及发展趋势进行了分析研究,认识到测区新构造运动由新第三纪—第四纪中更新世的间歇式掀起运动转化为晚更新世—早全新世的相对稳定,至全新世晚期转化为颤动性单陷运动的演化过程,并且其活动强度由老至新处于加强的趋势。这种运动特征对石臼港的发展建设是十分有利的。
According to the geological and geomorphological survey data of the hydrogeological survey of water supply in Shijiugang District of Shandong Province in 1984 and the drilling data of the Second Geological Unit of Shandong Bureau of Geology and Mineral Resources, the author analyzes the performance, type, intensity and development of neotectonic movement in the survey area The trend was analyzed and realized that the neotectonic movement of the survey area was transformed from the mid-Pleistocene intermittent setting-up movement of the Neogene to the late Pleistocene-Early Holocene to the stabilization of the late Holocene into tremor Sexual monotonous movement of the evolution process, and its activity intensity from old to new in the strengthening trend. This sporting characteristics of Shijiu Hong Kong’s development and construction is very favorable.