Origin of Silicate Spherules and Geochemistry of Re and Platinum-Group Elements Within Microfossil-Bearing Archean Chert from the 3.4 Ga Strelley Pool Formation, Western Australia

Author:

Sugitani Kenichiro1ORCID,Mimura Koichi1,Senda Ryoko2,Kouketsu Yui1,Wallis Simon13,Takagi Natsuko4,Iizuka Tsuyoshi3,Lowe Donald R.5

Affiliation:

1. Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan.

2. Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan.

3. Department of Earth and Planetary Science, The University of Tokyo, Tokyo, Japan.

4. Technical Center of Nagoya University, Nagoya, Japan.

5. Department of Geological Sciences, Stanford University, Stanford, California, USA.

Publisher

Mary Ann Liebert Inc

Subject

Space and Planetary Science,Agricultural and Biological Sciences (miscellaneous)

Reference77 articles.

1. Chemical nature of the 3.4 Ga Strelley Pool microfossils

2. Stromatolite reef from the Early Archaean era of Australia

3. Allwood AC, Burch I, and Walter MR (2007) Stratigraphy and Facies of the 3.43 Ga Strelley Pool Chert in the Southwestern North Pole Dome, Pilbara Craton, Western Australia. Geological Survey of Western Australia, Western Australia; Record 2007/11.

4. Spinel from Archean impact spherules

5. An Archean Impact Layer from the Pilbara and Kaapvaal Cratons

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