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Model of Reef Diagenesis: Mururoa Atoll, French Polynesia

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Reef Diagenesis

Abstract

Located within the Tuamotu Archipelago (Fig. 1), the Mururoa Atoll is characterized by an elongate morphology (25 × 9 km) which probably reflects the composite nature of its volcanic basement (Gachon 1985) situated at minimum depths of 180 m below lagoonal sea level and at depths varying between 350 and 450 m below peripheral islands (Buigues 1982). Radiometric datings (Labeyrie et al. 1969) indicate that volcanic activity ceased about 7 million years ago, approximately at the end of the Miocene. The considerable thickness of reefoid carbonates has been determined essentially by sustained Neogene subsidence of the Darwin ridge (Brousse 1985).

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Author information

Authors and Affiliations

  1. Laboratoire de Pétrologie Sédimentaire et Paléontologie, Université de Paris-Sud, Bâtiment 504, 91405, Orsay Cedex, France

    D. M. Aissaoui & B. H. Purser

  2. Commissariat à l’Energie Atomique, 91680, Bruyères-le-Châtel, France

    D. Buigues

Authors
  1. D. M. Aissaoui
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  2. D. Buigues
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  3. B. H. Purser
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Editor information

Editors and Affiliations

  1. George Washington University, Washington, USA

    Johannes H. Schroeder Ph.D.

  2. Institut für Geologie und Paläontologie, Technische Universität, Hardenbergstraße 42, 1000, Berlin 12, FR Germany

    Johannes H. Schroeder Ph.D.

  3. Laboratoire de Pétrologie Sédimentaire et Paléontologie, Université Paris-Sud Orsay, Bâtiment 504, 91405, Orsay Cedex, France

    Bruce H. Purser

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© 1986 Springer-Verlag Berlin Heidelberg

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Aissaoui, D.M., Buigues, D., Purser, B.H. (1986). Model of Reef Diagenesis: Mururoa Atoll, French Polynesia. In: Schroeder, J.H., Purser, B.H. (eds) Reef Diagenesis. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-82812-6_3

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  • DOI: https://doi.org/10.1007/978-3-642-82812-6_3

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-82814-0

  • Online ISBN: 978-3-642-82812-6

  • eBook Packages: Springer Book Archive

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