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Lithosphere Delamination with Foundering of Lower Crust and Mantle Caused Transient Uplift of Lord Howe Rise and Permanent Subsidence of New Caledonia Trough during Eocene and Oligocene Initiation of Tonga-Kermadec Subduction, Western Pacific

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Created 13/01/2025

Updated 13/01/2025

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We use seismic-reflection and rock-sample data to propose that the first-order physiography of New Caledonia Trough and Norfolk Ridge formed in Eocene to Miocene time, and was associated with the onset of subduction and back-arc spreading at the Australia-Pacific plate boundary. Our tectonic model involves an initial Cretaceous rift that is strongly modified by Cenozoic subduction initiation and hence we are able to explain: complex sedimentary basins of inferred Mesozoic age; a prominent unconformity and onlap surface of Middle Eocene to Early Miocene age at the base of flat-lying sediments beneath the axis of New Caledonia Trough; gently-dipping, variable thickness, and locally deformed Late Cretaceous strata along the margins of the trough; platform morphology and unconformities on either side of the trough that indicate a phase of Late Eocene to Early Miocene uplift to near sea level, followed by rapid Oligocene and Miocene subsidence of c. 1100-1800 m; and seismic-reflection facies tied to boreholes that suggest absolute tectonic subsidence at the southern end of New Caledonia Trough by 1800-2200 m since Eocene time. The Cenozoic part of the model involves delamination and subduction initiation followed by rapid foundering and rollback of the slab. This created a deep (>2 km) enclosed oceanic trough c. 2000 km long and 200-300 km across in Eocene and Oligocene time as the lower crust detached, with simultaneous uplift and local land development along basin flanks. Disruption of Late Cretaceous and Paleogene strata was minimal during this Cenozoic phase and involved only subtle tilting and local reverse faulting or folding. Basin formation was possible through the action of at least one detachment fault that allowed the lower crust to either be subducted into the mantle or exhumed eastward into Norfolk Basin. We suggest that delamination of the lithosphere, with possible mixing of the lower crust back into the mantle, is more widespread than previously thought.

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Title Lithosphere Delamination with Foundering of Lower Crust and Mantle Caused Transient Uplift of Lord Howe Rise and Permanent Subsidence of New Caledonia Trough during Eocene and Oligocene Initiation of Tonga-Kermadec Subduction, Western Pacific
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/e82eabd7-89cc-47f9-85c1-1b8be7861063
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[156.0, -35.0], [175.0, -35.0], [175.0, -13.75], [156.0, -13.75], [156.0, -35.0]]]}
Data Portal data.gov.au

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This dataset was originally found on data.gov.au "Lithosphere Delamination with Foundering of Lower Crust and Mantle Caused Transient Uplift of Lord Howe Rise and Permanent Subsidence of New Caledonia Trough during Eocene and Oligocene Initiation of Tonga-Kermadec Subduction, Western Pacific". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/lithosphere-delamination-with-foundering-of-lower-crust-and-mantle-caused-transient-uplift-of-l

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