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

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Published in P.Fenoll Hach-Ali, J. Torres-Ruiz, and F. Gervilla. Current research in geology applied to ore deposits. Proceedings of the Second Biennial SGA Meeting. Granada (Spain) - Sept. 9-13, 1993 - . 1993, p. 11-14
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"
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Structures
Research group Mineral Resources and Geofluids
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FONTBOTÉ, Lluis. Self-organization fabrics in carbonate-hosted ore deposits: the example of diagenetic crystallization rhythmites (DCRs). 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. Granada (Spain). [s.l.] : [s.n.], 1993. p. 11-14. https://archive-ouverte.unige.ch/unige:29376

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Deposited on : 2013-08-19

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