Applications of Magnetic Signature Monitoring in ODP
Magnetic signature monitoring of paleocllmate and sediment provenance has been more and more widely used in ODP studies and the achievements of these studies have aroused extensive concerns. In addition, magnetic monitoring of seafloor hydrothermal activity and gas hydrate has obtained some important achievements: (1) alteration degree of magnetic minerals is correlated with hydrothennal circulation of fluids; (2) formation of magnetic iron sulfides appears to correlate with the generation of gas hydrate, which provides a way by using magnetic methods to monitor gas hydrate distribution. But they are still in infancy and the detailed mechanism remains a topic for further research.
ODP magnetic tracing paleoclimate source monitroing gas hydrate seafloor hydrothennal activity.
Zhang Hongjie Xie Xinong Luo Miao Li Zhen Zhou Feng
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
国际会议
The IPACES 6th Annual Meeting(“现代地球科学，交流与合作国际学术研讨会暨第六届IPACES学术年会)
武汉
英文
16-18
2007-04-25（万方平台首次上网日期，不代表论文的发表时间）