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Diamond genesis in a multiply-constrained model

Nature volume 320, pages 34–38 (1986)Cite this article

Abstract

Thermal cracking of primordial carbon gas species in depleted and reduced Archaean subcratonic lithosphere is proposed for the nucleation of micro- and ultramafic macrodiamonds. Growth was mainly by solid-state diffusion, although crystallization of the eclogitic diamond suite was from sulphide-immiscible melts. Lateral and vertical heterogeneities and the geometry of the lithosphere can account for a variety of second-order variables such as diamond type, colour, crystal morphology and dissolution characteristics.

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Authors and Affiliations

  1. Department of Geology, University of Massachusetts, Amherst, Massachusetts, 01003, USA

    Stephen E. Haggerty

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Haggerty, S. Diamond genesis in a multiply-constrained model. Nature 320, 34–38 (1986). https://doi.org/10.1038/320034a0

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