摘要
本文根据中国海区及邻域的地磁场分布特征，结合地质及其它物探资料，对陆块碰撞过渡带的存在性问题、东沙—澎湖磁力高带的来源问题，东亚陆缘盆地磁异常分异的原因问题进行了讨论。
Based on magnetic field characteristics of China Seas and adjacent regions,together with geologic and other geophysical data,this paper discusses the subjects about the existence of transitional zone of continent continent collision,the origin of high magnetic anomaly belt in Dongsha Islands-Penghu Islands and the reason for different magnetic anomalies of marginal basins in East Asiaand finally divides the basement of China Seas and adjacent regions into six rock facies areas.
出处
《海洋地质与第四纪地质》
CAS
CSCD
北大核心
1997年第2期63-72,共10页
Marine Geology & Quaternary Geology
关键词
地磁场
渤海
黄海
基底岩相区
海区
China Seas and adjacent regions magnetic field division of basement
