Work Description

Title: Low-Fe(III) Greenalite Was a Primary Mineral from Neoarchean Oceans (Raw Data) Open Access Deposited

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Attribute Value
Methodology
  • X-ray absorption data was collected at the Canadian Light Source (CLS) and the Stanford Synchrotron Radiation Lightsource (SSRL). X-ray diffraction data collected at the United States Geological Survey in Boulder.
Description
  • Note: The "Readme_Metadata" file was updated on March 15, 2018 to include a citation to the related article making use of this data and was reformatted to be presented as a pdf file rather than as a docx file.

  • This data set is comprised of synchrotron-based X-ray transmission and absorption spectroscopy data as well as X-ray diffraction patterns that were performed to characterize the best-preserved examples of nanoscale iron silicate mineral inclusions from 2.5 billion-year-old Banded Iron Formations (BIFs) and ferruginous cherts.
Creator
Depositor
  • jenaje@umich.edu
Contact information
Discipline
Funding agency
  • Other Funding Agency
Keyword
Resource type
Last modified
  • 11/04/2019
Published
  • 02/15/2018
Language
DOI
  • https://doi.org/10.7302/Z2XS5SMK
License
To Cite this Work:
Johnson, J. E. (2018). Low-Fe(III) Greenalite Was a Primary Mineral from Neoarchean Oceans (Raw Data) [Data set], University of Michigan - Deep Blue Data. https://doi.org/10.7302/Z2XS5SMK

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