Start of the Wilson Cycle at 3 Ga Shown by Diamonds from Subcontinental Mantle

Author:

Shirey Steven B.1,Richardson Stephen H.2

Affiliation:

1. Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA.

2. Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa.

Abstract

Mineral inclusions in diamonds reveal that the modern pattern of continent movements began around 3 billion years ago.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference34 articles.

1. Static or mobile Earth: The current scientific revolution;Wilson J. T.;Proc. Am. Philos. Soc.,1968

2. The late Archean record: a puzzle in ca. 35 pieces

3. Plate Tectonics, the Wilson Cycle, and Mantle Plumes: Geodynamics from the Top

4. Precambrian palaeomagnetic results compatible with contemporary operation of the Wilson cycle

5. P. Hoffman in The Continental Crust and Its Mineral Deposits D. W. Strangway Ed. : Geol. Assoc. Canada Spec. Pap. 20 (1980) pp. 523–549.

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