关于现代海底热液活动系统模式的思考

王淑杰; 翟世奎; 于增慧; 国坤; 张侠

doi:10.3799/dqkx.2018.907

Volume 43 Issue 3

Mar. 2018

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Article Navigation > Earth Science > 2018 > 43(3): 835-850

Wang Shujie, Zhai Shikui, Yu Zenghui, Guo Kun, Zhang Xia, 2018. Reflections on Model of Modern Seafloor Hydrothermal System. Earth Science, 43(3): 835-850. doi: 10.3799/dqkx.2018.907

Citation:

Wang Shujie, Zhai Shikui, Yu Zenghui, Guo Kun, Zhang Xia, 2018. Reflections on Model of Modern Seafloor Hydrothermal System. Earth Science, 43(3): 835-850. doi: 10.3799/dqkx.2018.907

Wang Shujie, Zhai Shikui, Yu Zenghui, Guo Kun, Zhang Xia, 2018. Reflections on Model of Modern Seafloor Hydrothermal System. Earth Science, 43(3): 835-850. doi: 10.3799/dqkx.2018.907

Citation:

Wang Shujie, Zhai Shikui, Yu Zenghui, Guo Kun, Zhang Xia, 2018. Reflections on Model of Modern Seafloor Hydrothermal System. Earth Science, 43(3): 835-850. doi: 10.3799/dqkx.2018.907

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Reflections on Model of Modern Seafloor Hydrothermal System

doi: 10.3799/dqkx.2018.907

1.
Center of Deep Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266001, China
2.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Key Lab of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

Received Date: 2017-11-23
Publish Date: 2018-03-15

Abstract

Abstract

Modern seafloor hydrothermal activity is generally accompanied by magmatism. Traditional hydrothermal system model hypothesizes that seawater penetrates through the rifts or cracks, then is heated and reacts with the surrounding rocks gradually leaching out metal elements from the rocks and resulting in the formation of metal-rich, acidic and reductive hydrothermal fluid. Subsequently, the heated fluid moves up along a series of fissures and erupts directly out of the ocean floor leading to precipitations of hydrothermal sulfides.This model reasonably accounts for the existence of fluid, channels and heat sources which are the three fundamental elements of modern seafloor hydrothermal system, and is in accord with many phenomena we have observed so far. However, differences in rock permeability, hydrothermal fluid properties, thermal fluid ecosystem and hydrothermal product indicate that there is possibly another injected circulation pattern for modern seafloor hydrothermal systems, which means the hydrothermal fluid is derived from the direct injection of fluid and volatile components from the deep magma chamber. Accordingly, it is inferred that there possibly are two models for modern seafloor hydrothermal systems:one is the shallow circulation mode, namely the traditional mode of hydrothermal circulation; the other is a magmatic hydrothermal injection mode ("injection model"). In the environment of strong magmatism and well-developed fracture, two modes may exist simultaneously, and the double diffusive convection circulation model is proposed. The double diffusive convection circulation model can be used to explain a variety of phenomena and facts recently discovered in the study of modern seafloor hydrothermal system. Moreover, it is pointed out that the tectonic background of the subduction and the mixing of materials from both subduction component and continental crust are also considered in the study of the magmatism and hydrothermal activity in back-arc basin. Meanwhile, a theoretical model has been constructed for the sea-floor hydrothermal system in back-arc basin taking the Okinawa trough as an example.
- magmatism,
- seafloor hydrothermal system,
- double diffusive convection system model,
- back-arc basin,
- Okinawa trough

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References(150)

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Reflections on Model of Modern Seafloor Hydrothermal System

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