Natural fluid-deposited graphite; mineralogical characteristics and mechanisms of formation

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ID: 292771
1998
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Abstract
This paper focuses on the similarities and differences between metamorphic graphite (formed in situ from organic matter) and fluid-deposited graphite. We discuss the formation of fluid-deposited graphite in terms of the source of carbon, the characteristics of the C-bearing fluids (the C-O-H system), the mechanisms of carbon mobilization, and the mechanisms of carbon precipitation. New and existing analytical data are compiled on the physical and chemical characteristics of fluid-deposited graphite obtained by the following techniques: optical microscopy, differential thermal analysis, thermogravimetry, X-ray diffraction, Raman spectroscopy, and stable isotope mass spectrometry. Our discussions focus on major, that is, volumetrically significant, worldwide concentrations of graphite.
Reference Key
openalex_W1997982498 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Francisco Javier Luque del Villar, Jill Dill Pasteris, B. Wopenka, M. Rodas, José F. Barrenechea
Journal american journal of science
Year 1998
DOI
10.2475/ajs.298.6.471
URL
https://ajsonline.org/article/60786.pdf
Keywords Keywords not found

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