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利用数字地震仪、地质脉冲仪和3.5kH_Z真浅层剖面仪测量结果显示:南黄海地层可分为三个大层组,即第四系、上第三系和下第三系(或第三系以前的地层)。它们分别沉积在南、北两个沉积中心中,这两个沉积中心始终控制着盆地的沉积。在盆地发展过程中,西部大陆的物质一直是盆地沉积的主要物质来源。第四纪时,黄河已经显示了它对南黄海影响的主导地位。无论是第三纪还是第四纪沉积物均以陆相为主。第四纪的地质历史是复杂多变的,至少有两次以上的成陆过程。
The results of digital seismograph, geo-pulsator and 3.5kHZ true superficial profiler show that the South Yellow Sea can be divided into three large layers, that is, Quaternary, Upper Tertiary and Lower Tertiary (or third Former strata). They were deposited in the two south and north depositional centers, both of which controlled the sedimentation of the basin. During the development of the basin, the material of the western mainland has been the main source of sediments in the basin. Quaternary, the Yellow River has shown its dominance of the impact of the South Yellow Sea. Whether the Tertiary or Quaternary sediments are mainly continental. Quaternary geological history is complex and changeable, at least twice more into the land process.