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TAO Chunhui,WU Guanghai,DENG Xianming,QIU Zhongyan,HAN Chenhua,LONG Yanmei. 2013. New discovery of seafloor hydrothermal activity on the Indian Ocean Carlsberg Ridge and Southern North Atlantic Ridge—progress during the 26th Chinese COMRA cruise. Acta Oceanologica Sinica, 32(8):85-88
New discovery of seafloor hydrothermal activity on the Indian Ocean Carlsberg Ridge and Southern North Atlantic Ridge—progress during the 26th Chinese COMRA cruise
Received:January 01, 2013  Revised:June 18, 2013
DOI:10.1007/s13131-013-0345-x
Key words:26th COMRA cruise  Carlsberg Ridge  IndianOcean,North AtlanticRidge  seafloor hydrothermal activity
中文关键词:  
基金项目:the National Basic Research Program of China under contract No. 2012CB417305; China Ocean Mineral Resources Research & Development Association Project under contract No. DY125-11; Endowment Fund of International Seabed Authority (the International Cooperative Study on Hydrothermal System at Ultraslow Spreading SWIR).
Author NameAffiliationE-mail
TAO Chunhui Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China  
WU Guanghai Key Laboratory of Marine Ecosystemand Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China wugh6866@yahoo.com.cn 
DENG Xianming Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China  
QIU Zhongyan Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China  
HAN Chenhua Key Laboratory of Marine Ecosystemand Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China  
LONG Yanmei State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State  
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Abstract:
      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 3.5°-3.8°Non 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 4°-7°N. The discovery of two hydrothermal and anomaly fields filled in the gap of hydrothermal investigation and study in the corresponding regions for China.
中文摘要:
      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 3.5°-3.8°Non 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 4°-7°N. The discovery of two hydrothermal and anomaly fields filled in the gap of hydrothermal investigation and study in the corresponding regions for China.
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