Work Description

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

http://creativecommons.org/licenses/by-nc/4.0/
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
Citations to related material
  • Johnson, J. E., Muhling, J. R., Cosmidis, J., Rasmussen, B. & Templeton, A. S. (2018). Low-Fe(III) Greenalite Was a Primary Mineral from Neoarchean Oceans. Geophysical Research Letters, 45. https://doi.org/10.1002/2017GL076311
Resource type
Last modified
  • 11/04/2019
Published
  • 02/15/2018
Language
DOI
License
To Cite this Work:
Johnson, J. (2018). Low-Fe(III) Greenalite Was a Primary Mineral from Neoarchean Oceans (Raw Data) [Data set]. University of Michigan - Deep Blue. https://doi.org/10.7302/Z2XS5SMK

Relationships

Files (Count: 4; Size: 70.5 MB)

Thumbnail Title Original Upload Last Modified File Size Access Actions
44558d88m?file=thumbnail ReadMe_Metadata.pdf 2018-03-15 2018-03-15 74.1 KB Open Access
Default CLS STXM raw data.zip 2018-02-15 2018-02-15 19.3 MB Open Access
Default SSRL XAS raw data.zip 2018-02-15 2018-02-15 51 MB Open Access
Default XRD raw data.zip 2018-02-15 2018-02-15 31.6 KB Open Access

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