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  • 标题:A demonstration of an affinity between pyrite and organic matter in a hydrothermal setting
  • 本地全文:下载
  • 作者:Paula Lindgren ; John Parnell ; Nils G Holm
  • 期刊名称:Geochemical Transactions
  • 电子版ISSN:1467-4866
  • 出版年度:2011
  • 卷号:12
  • 期号:1
  • 页码:1-7
  • DOI:10.1186/1467-4866-12-3
  • 出版社:BioMed Central
  • 摘要:One of the key-principles of the iron-sulphur world theory is to bring organic molecules close enough to interact with each other, using the surface of pyrite as a substrate in a hydrothermal setting. The present paper explores the relationship of pyrite and organic matter in a hydrothermal setting from the geological record; in hydrothermal calcite veins from Carboniferous limestones in central Ireland. Here, the organic matter is accumulated as coatings around, and through, pyrite grains. Most of the pyrite grains are euhedral-subhedral crystals, ranging in size from ca 0.1-0.5 mm in diameter, and they are scattered throughout the matrix of the vein calcite. The organic matter was deposited from a hydrothermal fluid at a temperature of at least 200°C, and gives a Raman signature of disordered carbon. This study points to an example from a hydrothermal setting in the geological record, demonstrating that pyrite can have a high potential for the concentration and accumulation of organic materials.
  • 关键词:Calcite;Pyrite;Bitumen;Fluid Inclusion;Hydrothermal Fluid
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