First active hydrothermal vents on an ultraslow-spreading center: Southwest Indian Ridge

Author:

Tao Chunhui1,Lin Jian2,Guo Shiqin3,Chen Yongshun John4,Wu Guanghai1,Han Xiqiu1,German Christopher R.2,Yoerger Dana R.5,Zhou Ning3,Li Huaiming1,Su Xin6,Zhu Jian4,

Affiliation:

1. Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, SOA, Hangzhou 310012, China

2. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA

3. China Ocean Mineral Resources R&D Association, Beijing 100860, China

4. Department of Geophysics, School of Earth & Space Sciences, Peking University, Beijing 100871, China

5. Department of Applied Physics and Ocean Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA

6. China University of Geosciences, School of Ocean Sciences, Beijing 100083, China

Publisher

Geological Society of America

Subject

Geology

Reference30 articles.

1. Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°–16°E: Geochemistry, Geophysics;Bach;Geosystems,2002

2. On the global distribution of hydrothermal vent fields;Baker,2004

3. Hydrothermal venting in magma deserts: The ultraslow-spreading Gakkel and Southwest Indian Ridges;Baker;Geochemistry, Geophysics, Geosystems,2004

4. Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR);Charlou;Chemical Geology,2002

5. Handbook of Deep-Sea Hydrothermal Vent Fauna (2nd Completely Revised Edition);Desbruyeres,2006

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