the history of studies on seafloor hydrothermal activity and several important issues being researched at present are reviewed.
本文简要介绍了海底热液活动的研究历史,以及目前研究的几个主要问题。
seafloor hydrothermal system mainly distributes in the tensile environment such as mor, arc-rear basin, intraplate volcanic center and so on.
海底热液系统主要分布在大洋中脊、弧后盆地、板内火山活动中心等张裂性环境中,不同的环境具有类似的成矿模式。
studies on seafloor hydrothermal sulfides and its ore-forming processes;
科学家们确信在海底下方的热点作用。
in the paper, directions and results of the study on modern seafloor hydrothermal activity are analyzed and summarized firstly.
本文首先对现代海底热液活动的研究现状,包括业已取得的主要研究成果和主要研究方向进行了分析总结。
another advance is that the observation and investigation of seafloor hydrothermal processes and mineralization provide invaluable information for understanding the origin of ancient vms deposits.
现代海底热水成矿作用观察和研究为古代vms矿床成因研究提供了重要信息,对现有成矿理论产生重要影响。
modern seafloor hydrothermal process is an important ore-forming process.
现代海底热液成矿作用是一种重要的成矿作用。
study on control technology of self-calibration for seafloor hydrothermal fluid ph exploration electrode;
介绍了国外在现代海底热液活动调查研究中使用的方法和技术手段 。
seafloor hydrothermal activities have been found in tbe red sea, galapagos, east pacific rise, gulf of california, and mid-atlantic ridge since 1960s.
六十年代以来,在红海、加拉帕果斯、东太平洋隆起、加利福尼亚湾以及大西洋中脊等地发现了海底热液活动并有富含重金属的沉积物形成。