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CM41_1049.pdf
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Dendritic magnetite and ilmenite crystals were found in 590 Ma Grenville dikes near Otter Lake, Quebec, Canada. The magnetite dendrites have complex shapes with three intersecting primary plates and secondary arrowhead plates, while ilmenite dendrites consist of thin interconnected plates. The growth of these dendrites is attributed to temperature and concentration gradients in the melt, as well as the tendency to form specific crystal planes. The cooling rates in the small dikes where these dendrites were found are estimated to be between 0.6 and 60°C per hour.

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Dendritic magnetite and ilmenite crystals were found in 590 Ma Grenville dikes near Otter Lake, Quebec, Canada.

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  • File Format: PDF
  • File Size: 568 KB
  • Pages: 11
  • Language: EN
  • Total Downloads: 92
  • Last Updated: 1 week ago

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