Distribution Pattern of Submarine Hydrothermal Sulfide Deposits and Controlling Factors
详细信息
- 责任者：Jing Chunlei (First Institute of Oceanography ; State Oceanic Administration ; Qingdao 266061 ; China) ; Zheng Yanpeng
- 刊名：Marine Geology & Quaternary Geology
- 出版年：2013
- 卷期：33(1)
- 关键词：热液矿床 ; hydrothermal deposit ; 多金属矿 ; polymetallic ores
- 页码：p.57-64
- 图表：illus., 2 tables, 41 refs.
- 分类号：1001
- issnNo：ISSN0256-1492
- isbnNo：CN37-1117/P
摘要
The latest data on global hydrothermal vent sites are used in this paper to discuss the tectonic settings of submarine polymetallic sulfide deposits and other ore-controlling factors,such as the deep magmatic activity,fault structure and sediment cap.Results show that the submarine hydrothermal polymetallic sulfide vent sites are mainly located at the divergent and convergent plate boundaries;the deep magmatic activity and the fault structures are the most important factors controlling the distribution of the hydrothermal polymetallic sulfide on mid-ocean ridges;and the speed of sea floor spreading contributes to the size of polymetallic sulfide deposits.Conclusions of this study could be used as the reference in the exploration of submarine hydrothermal polymetallic resources.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |