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布拜图对热液氧化物沉淀条件的指示 被引量:1

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摘要 无定形Fe-和Mn-羟基氧化物以及硅的沉积体广泛分布于洋中脊(Dekov et al.,2010)、弧后盆地(Hein et al.,2008;Zeng et al.,2012)和海山(Emerson et al.,2002;Edwards et al.,2011)等不同地质背景的海底热液区。热液Fe-羟基氧化物按成因可以分为三类:热液硫化物的氧化产物。
出处 《矿物学报》 CAS CSCD 北大核心 2013年第S2期676-677,共2页 Acta Mineralogica Sinica
基金 国家重点基础研究发展计划(973计划)项目(批准号:2013CB429700)
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