中国陆架海绿石分布特征及其意义  

DISTRIBUTION PROPERTIES OF GLAUCONITES IN CHINESE SHELF SEA AND THEIR SIGNIFICANCE

作　　者：赵全基[1] 彭汉昌[1] 张壮域 

机构地区：[1]国家海洋局第一海洋研究所,青岛266003

出　　处：《海洋科学》1992年第5期41-44,共4页Marine Sciences

摘　　要：本文根据实际资料,简要概括了中国大陆架海绿石的分布规律和形成环境。海绿石的富集区与氧化环境,粗粒沉积和残留沉积区相一致。该研究为恢复古沉积环境提供了依据。In this paper, the distribution regularity and growth environment of glauconites were summarized briefly on the basis of a number of real data. We found that concentration areas of .glauconites are identicalwith the oxidizing environment, coarse-sediment areas and relict sediments. This study provided theevidence for resumption of ancient sedimentation environment.

关 键 词：陆架 海绿石 分布 

分 类 号：P578.963[天文地球—矿物学]