New discovery of seafloor hydrothermal activity on the Indian Ocean Carlsberg Ridge and Southern North Atlantic Ridge-progress during the 26th Chinese COMRA cruise

被引:16
作者
Tao Chunhui [1 ]
Wu Guanghai [2 ]
Deng Xianming [1 ]
Qiu Zhongyan [1 ]
Han Chenhua [2 ]
Long Yanmei [3 ]
机构
[1] State Ocean Adm, Inst Oceanog 2, Key Lab Submarine Geosci, Hangzhou 310012, Zhejiang, Peoples R China
[2] State Ocean Adm, Inst Oceanog 2, Key Lab Marine Ecosyst & Biogeochem, Hangzhou 310012, Zhejiang, Peoples R China
[3] State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China
关键词
26th COMRA cruise; Carlsberg Ridge; Indian Ocean; North Atlantic Ridge; seafloor hydrothermal activity; RODRIGUEZ TRIPLE JUNCTION; PLUMES; EVENT; VENTS;
D O I
10.1007/s13131-013-0345-x
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The 26th Chinese COMRA (China Ocean Mineral Resources Research & Development Association) cruise was an important cruise. The Carlsberg Ridge (CR) of the Northwest Indian Ocean and the North Atlantic Ridge (NAR), in which less investigation has been carried out for hydrothermal activities, were investigated and studied during the first two legs of the 26th COMRA cruise. During the first leg, we found one hydrothermal activity field located in the CR at 3.5A degrees-3.8A degrees N on the Northwest Indian Ocean Ridge (NWIR), and sampled seafloor polymetallic sulfide deposits where only abnormalities were found before. During the second leg, we found a new hydrothermal anomaly field located in the NAR at 4A degrees-7A degrees N. The discovery of two hydrothermal and anomaly fields filled in the gap of hydrothermal investigation and study in the corresponding regions for China.
引用
收藏
页码:85 / 88
页数:4
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