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Monitoring and observatories: Multidisciplinary, Time-Series Observations at Mid-Ocean Ridges

机译:监测和观测站:大洋中脊的多学科时间序列观测

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摘要

Mid-ocean ridges represent one of the few environments where it is possible to directly and regularly observe the connectivity among tectonic, volcanic, geochemical, and biological processes. This interaction of life and earth processes related to crustal accretion has provided a focus for a great deal of interdisciplinary research since the discovery of seafloor hydrothermalism in 1977 (Lonsdale, 1977). Exploration and comparison of spreading ridges and hydrothermal systems in different areas of the world continue to advance understanding of cause-and-effect relationships.
机译:中海洋脊是少数几个可以直接并定期观察构造,火山,地球化学和生物过程之间的连通性的环境之一。自1977年发现海底热液作用以来,与地壳积聚相关的生命与地球过程的这种相互作用为众多跨学科研究提供了关注点(Lonsdale,1977)。在世界不同地区,对扩张脊和热液系统的探索和比较将继续加深对因果关系的理解。

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