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THE FORMATION OF ORES IN THE SEDIMENTARY ENVIRONMENT OF THE DEEP SEA WITH MICROBIAL PARTICIPATIONTHE CASE FOR FERROMANGANESE CONCRETIONS

 

作者: HENRY EHRLICH,  

 

期刊: Soil Science  (OVID Available online 1975)
卷期: Volume 119, issue 1  

页码: 36-41

 

ISSN:0038-075X

 

年代: 1975

 

出版商: OVID

 

数据来源: OVID

 

摘要:

Ferromanganese concretions and crusts on the floor of the deep sea are discussed as examples of ores formed in the marine sedimentary environment of the oceans. Their properties, the origin of their constituents, and their mode of formation, including the role of microbes in this process, are considered.

 

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