~3,000 Ma, Cleaverville Formation, Cleaverville Greenstone Belt, West Pilbara, Western Australia

Part of the Topics in Geobiology book series (TGBI, volume 31)


Zircon Sandstone Geochemistry Beach Lamination 


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Recommended Reading

  1. Hickman, A. H., Smithies, R. H., Pike, G., Farrell, T. R., and Beintema, K. A., 2001, Evolution of the West Pilbara granite-greenstone terrane and Mallina Basin, Western Australia—a field guide, Western Australia Geological Survey Record 2001/16: 63p.Google Scholar
  2. Kiyokawa, S., and Taira, A., 1998, The Cleaverville Group in the West Pilbara coastal granitoid-greenstone terrain of Western Australia: an example of a Mid-Archaean immature oceanic island-arc succession, Precambrian Research 88: 109–142.CrossRefGoogle Scholar
  3. Ohta, H., Maruyama, S., Takahashi, E., and Kato, Y. , 1996, Field occurrence, geochemistry, and petrogenesis of the Archean Mid-Oceanic Ridge Basalts (AMORBs) of the Cleaverville area, Pilbara craton, Western Australia, Lithos 37: 199–221.CrossRefGoogle Scholar
  4. Ueno, Y. , Isozaki, Y. , and McNamara, K.J., 2006, Coccoid-like microstructures in a 3.0 Ga chert from Western Australia, International Geology Review 48: 78–88.CrossRefGoogle Scholar

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