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Subsidence and uplift by slab-related mantle dynamics: a driving mechanism for the Late Cretaceous and Cenozoic evolution of continental SE Asia?

Benjamin Clements, Peter M. Burgess, Robert Hall and Michael A. Cottam
Geological Society, London, Special Publications, 355, 37-51, 1 January 2011, https://doi.org/10.1144/SP355.3
Benjamin Clements
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UKStatoil ASA, Forusbeen 50, N-4035 Stavanger, Norway
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Peter M. Burgess
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Robert Hall
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Michael A. Cottam
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Abstract

Continental SE Asia is the site of an extensive Cretaceous–Paleocene regional unconformity that extends from Indochina to Java, covering an area of c. 5 600 000 km2. The unconformity has previously been related to microcontinental collision at the Java margin that halted subduction of Tethyan oceanic lithosphere in the Late Cretaceous. However, given the disparity in size between the accreted continental fragments and area of the unconformity, together with lack of evidence for requisite crustal shortening and thickening, the unconformity is unlikely to have resulted from collisional tectonics alone. Instead, mapping of the spatial extent of the mid–Late Cretaceous subduction zone and the Cretaceous–Paleocene unconformity suggests that the unconformity could be a consequence of subduction-driven mantle processes. Cessation of subduction, descent of a northward dipping slab into the mantle, and consequent uplift and denudation of a sediment-filled Late Jurassic and Early Cretaceous dynamic topographic low help explain the extent and timing of the unconformity. Sediments started to accumulate above the unconformity from the Middle Eocene when subduction recommenced beneath Sundaland.

  • © The Geological Society of London 2011
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Geological Society, London, Special Publications: 355 (1)
Geological Society, London, Special Publications
Volume 355
2011
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Subsidence and uplift by slab-related mantle dynamics: a driving mechanism for the Late Cretaceous and Cenozoic evolution of continental SE Asia?

Benjamin Clements, Peter M. Burgess, Robert Hall and Michael A. Cottam
Geological Society, London, Special Publications, 355, 37-51, 1 January 2011, https://doi.org/10.1144/SP355.3
Benjamin Clements
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UKStatoil ASA, Forusbeen 50, N-4035 Stavanger, Norway
  • Find this author on Google Scholar
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  • For correspondence: becl@statoil.com
Peter M. Burgess
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Robert Hall
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Michael A. Cottam
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
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Subsidence and uplift by slab-related mantle dynamics: a driving mechanism for the Late Cretaceous and Cenozoic evolution of continental SE Asia?

Benjamin Clements, Peter M. Burgess, Robert Hall and Michael A. Cottam
Geological Society, London, Special Publications, 355, 37-51, 1 January 2011, https://doi.org/10.1144/SP355.3
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  • Article
    • Abstract
    • Expected styles of uplift: collisional- v. mantle-driven
    • Sundaland: continental SE Asia
    • Evidence for Cretaceous subduction and collision in SE Asia
    • A Late Cretaceous to Eocene unconformity
    • Testing the hypothesis: an unconformity due to dynamic topography
    • Conclusions
    • Acknowledgments
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