A

Mass transfer into the leading edge of the mantle wedge: Initial results from Oman Drilling Project Hole BT1B

Abstract

This paper provides an overview of research on core from Oman Drilling Project Hole BT1B and the surrounding area, plus new data and calculations, constraining processes in the Tethyan subduction zone beneath the Samail ophiolite. The area is underlain by gently dipping, broadly folded layers of allochthonous Hawasina pelagic sediments, the metamorphic sole of the Samail ophiolite, and Banded Unit peridotites at the base of the Samail mantle section. Despite reactivation of some faults during uplift of the Jebel Akdar and Saih Hatat domes, the area preserves the tectonic “stratigraphy” of the Cretaceous subduction zone. Gently dipping listvenite bands, parallel to peridotite banding and to contacts between the peridotite and the metamorphic sole, replace peridotite at and near the basal thrust. Listvenites formed at less than 200°C and (poorly constrained) depths of 25 to 40 km by reaction with CO 2 -rich, aqueous fluids migrating from greater depths, derived from devolatilization of subducting sediments analogous to clastic sediments in the Hawasina Formation, at 400-500°. Such processes could form important reservoirs for subducted CO 2 . Listvenite formation was accompanied by ductile deformation of serpentinites and listvenites – perhaps facilitated by fluid-rock reaction – in a process that could lead to aseismic subduction in some regions. Addition of H 2 O and CO 2 to the mantle wedge, forming serpentinites and listvenites, caused large increases in the solid mass and volume of the rocks. This may have been accommodated by fractures formed as a result of volume changes, perhaps mainly at a serpentinization front.

Authors 23

  1. P. B. Kelemen corresponding

    Columbia University

    Affiliation as printed

    Columbia University

  2. University of Calgary

    Affiliation as printed

    University of Calgary

  3. Lamont-Doherty Earth Observatory

    Affiliation as printed

    Lamont Doherty Earth Observatory

  4. Université de Montpellier

    Affiliation as printed

    Universite de Montpellier

  5. Japan Agency for Marine-Earth Science and Technology

    Affiliation as printed

    Japan Agency for Marine-Earth Science and Technology

  6. McGill University

    Affiliation as printed

    McGill University

  7. University of California, Los Angeles

    Affiliation as printed

    University of California Los Angeles

  8. Affiliation as printed

    University of Colorado

  9. RWTH Aachen University

    Affiliation as printed

    RWTH Aachen University

  10. RWTH Aachen University

    Affiliation as printed

    RWTH Aachen University

  11. Brown University

    Affiliation as printed

    Brown University

  12. University of California, Santa Barbara

    Affiliation as printed

    University of California, Santa Barbara

  13. The University of Texas at Austin

    Affiliation as printed

    University of Texas at Austin

  14. Université de Montpellier

    Affiliation as printed

    University of Montpellier

  15. University of Bergen

    Affiliation as printed

    University of Bergen

  16. National Oceanography Centre

    Affiliation as printed

    National Oceanography Centre

  17. Affiliation as printed

    Alara Resources Ltd

  18. University of Southampton

    Affiliation as printed

    University of Southampton

  19. National Oceanography Centre

    Affiliation as printed

    National Oceanography Centre Southampton

  20. Nagoya University

    Affiliation as printed

    Nagoya University

  21. Niigata University

    Affiliation as printed

    Niigata University

  22. Affiliation as printed

    Oman Water Society

  23. University of Plymouth

    Affiliation as printed

    University of Plymouth

Cited by 8 stored of 8

8 results

No patents citing this paper on Lens.org (checked 2026-10-06).

References 0