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Self-organization fabrics in carbonate-hosted ore deposits: the example of diagenetic crystallization rhythmites (DCRs)

Contributors

Fontboté, Lluís

Presented at

Granada (Spain), Sept. 9-13, 1993

Published in

P.Fenoll Hach-Ali, J. Torres-Ruiz, and F. Gervilla (Ed.), Current research in geology applied to ore deposits. Proceedings of the Second Biennial SGA Meeting, p. 11-14

Publication date

1993

Abstract

Certain rhythmic fabrics described below and which are typical for many carbonate-hosted ore deposits are not determined by a possible original depositional or tectonic rhythmicity. It is rather suggested that they are due completely or in part to “self-organization” processes, i.e., ."the spontaneous transition of a non-equilibrium system from a non-patterned state to a patterned state without the intervention of patterned external cause"

UNIGE affiliation entities

UNIGE research groups

Citation (ISO format)

FONTBOTÉ, Lluís. Self-organization fabrics in carbonate-hosted ore deposits: the example of diagenetic crystallization rhythmites (DCRs). In: Current research in geology applied to ore deposits. Proceedings of the Second Biennial SGA Meeting. P.Fenoll Hach-Ali, J. Torres-Ruiz, and F. Gervilla (Ed.). Granada (Spain). [s.l.] : [s.n.], 1993. p. 11–14.

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Proceedings chapter (Accepted version)

Identifiers

  • PID : unige:29376
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Update

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