WANG Shaung, LIU Jian, LI Jianchao, QIU Jiandong. PROGRESS OF ENVIRONMENTAL MAGNETISM RESEARCH OF BOTTOM SEDIMENT IN EAST CHINESE CONTINENTAL SEAS[J]. Marine Geology & Quaternary Geology, 2016, 36(6): 85-94. DOI: 10.16562/j.cnki.0256-1492.2016.06.011
Citation: WANG Shaung, LIU Jian, LI Jianchao, QIU Jiandong. PROGRESS OF ENVIRONMENTAL MAGNETISM RESEARCH OF BOTTOM SEDIMENT IN EAST CHINESE CONTINENTAL SEAS[J]. Marine Geology & Quaternary Geology, 2016, 36(6): 85-94. DOI: 10.16562/j.cnki.0256-1492.2016.06.011

PROGRESS OF ENVIRONMENTAL MAGNETISM RESEARCH OF BOTTOM SEDIMENT IN EAST CHINESE CONTINENTAL SEAS

  • The East Chinese Continental Seas (ECCS) is a primary sink of sediments for Chinese rivers. These sediments bear abundant geological stories, and environmental magnetism, as an efficient and accurate research method, has its unique advantages in revealing these stories. By the environmental magnetism studies on sediment of ECCS, the distribution pattern of magnetic characteristics has so far been well recognized. And as an effective tool, environmental magnetism is of great indicative significance to tracing sedimentary provenance. In addition, some achievements in sedimentary redox environment reestablishment are also accomplished. Furthermore, environmental magnetism is also an indicator of heavy metals pollution and a basic tool for establishment of magnetostratigraphy and paleoclimate change, and has achieved great success. Thus, as a widely accepted geological research method, environmental magnetism is a significant supplement to traditional methods, and will provide new thoughts for future researches.
  • loading

Catalog

    Turn off MathJax
    Article Contents

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return