Data

The breakup of East Gondwana: A best-fit tectonic model

The University of Sydney
Dietmar Muller (Aggregated by, Associated with) Joanne Whittaker (Aggregated by) Whittaker, Jo (Aggregated by)
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.4227/11/5587A87EC4E5C&rft.title=The breakup of East Gondwana: A best-fit tectonic model&rft.identifier=http://dx.doi.org/10.4227/11/5587A87EC4E5C&rft.publisher=The University of Sydney&rft.description=This data collection is associated with the publication: Gibbons, A. D., Whittaker, J. M., & Müller, R. D. (2013). The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best-fit tectonic model. Journal of Geophysical Research: Solid Earth, 118(3), 808-822. doi: 10.1002/jgrb.50079Publication AbstractPublished models for the Cretaceous seafloor-spreading history of East Gondwana result in unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate particular constraints from at least one of the associated ocean basins. We link East Gondwana spreading corridors by integrating magnetic and gravity anomaly data from the Enderby Basin off East Antarctica within a regional plate kinematic framework to identify a conjugate series of east-west-trending magnetic anomalies, M4 to M0 (~126.7–120.4 Ma). The mid-ocean ridge that separated Greater India from Australia-Antarctica propagated from north to south, starting at ~136Ma northwest of Australia, and reached the southern tip of India at ~126 Ma. Seafloor spreading in the Enderby Basin was abandoned at ~115 Ma, when a ridge jump transferred the Elan Bank and South Kerguelen Plateau to the Antarctic plate. Our revised plate kinematic model helps resolve the problem of successive two-way strike-slip motion between Madagascar and India seen in many previously published reconstructions and also suggests that seafloor spreading between them progressed from south to north from 94 to 84 Ma. This timing is essential for tectonic flow lines to match the curved fracture zones of the Wharton and Enderby basins, as Greater India gradually began to unzip from Madagascar from ~100 Ma. In our model, the 85-East Ridge and Kerguelen Fracture Zone formed as conjugate flanks of a “leaky” transform fault following the ~100Ma spreading reorganization. Our model also identifies the Afanasy Nikitin Seamounts as products of the Conrad Rise hotspot.Authors and InstitutionsAna D. Gibbons - EarthByte Research Group, School of Geosciences, The University of Sydney, AustraliaJoanne M. Whittaker - EarthByte Research Group, School of Geosciences, The University of Sydney, Australia. ORCID: 0000-0002-3170-3935R. Dietmar Müller - EarthByte Research Group, School of Geosciences, The University of Sydney, Australia. ORCID: 0000-0002-3334-5764Overview of Resources ContainedThis data collection includes the all of the files needed to visualise, recreate, and interact with the plate motion model developed and published in Gibbons et al. (2013). Data used in the development of the plate motion model are also included.List of ResourcesNote: For details on the files included in this data collection, see “Description_of_Resources.txt”.Note: For information on file formats and what programs to use to interact with various file formats, see “File_Formats_and_Recommended_Programs.txt”.Rotation file for the tectonic model (.rot, 537 KB)Continent-ocean boundary geometries (.gpml, .kml, .txt, .shp, total 684 KB)Extinct ridge geometries (.gpml, .kml, .txt, .shp, total 414 KB)Fracture zone geometries (.gpml, .kml, .txt, .shp, total 6.8 MB)Isochron geometries (.gpml, .kml, .txt, .shp, total 4 MB)Large igneous province outlines (.gpml, .kml, .txt, .shp, total 279 KB)Magnetic anomaly picks (.gpmlz, .kml, .txt, .shp, total 17.5 MB)For more information on this data collection, and links to other datasets from the EarthByte Research Group please visit EarthByteFor more information about using GPlates, including tutorials and a user manual please visit GPlates or EarthByte&rft.creator=Dietmar Muller&rft.creator=Joanne Whittaker&rft.creator=Whittaker, Jo&rft.date=2015&rft.relation=http://doi.org/10.1002/jgrb.50079&rft.coverage=East Gondwana&rft.coverage=Indian Ocean&rft.coverage=Bounding Box: 30N, 6W; 60S, 6W; 60S, 160E; 30N, 160E&rft.coverage=-5.9027222264561,-60.074047321703 -5.9027222264561,30.432764808463 160.73790277355,30.432764808463 160.73790277355,-60.074047321703 -5.9027222264561,-60.074047321703&rft_rights=CC BY: Attribution 3.0 AU http://creativecommons.org/licenses/by/3.0/au&rft_subject=Indian Ocean&rft_subject=Kerguelen Plateau&rft_subject=Madagascar&rft_subject=Australia&rft_subject=East Antarctica&rft_subject=85-East Ridge&rft_subject=Afanasy Nikitin Seamounts&rft_subject=Conrad Rise hotspot&rft_subject=magnetic anomalies&rft_subject=seafloor-spreading&rft_subject=ridge jump&rft_subject=plate kinematics&rft_subject=mid-ocean ridges&rft_subject=transform faults&rft_subject=fracture zones&rft_subject=plate reorganisations&rft_subject=Cretaceous&rft_subject=Cenozoic&rft_subject=GPlates&rft_subject=plate motion model&rft_subject=plate boundaries&rft_subject=East Gondwana&rft_subject=Greater India&rft_subject=Enderby Basin&rft_subject=Wharton Basin&rft_subject=Elan Bank&rft_subject=Tectonics&rft_subject=EARTH SCIENCES&rft_subject=GEOLOGY&rft_subject=Marine Geoscience&rft_subject=Geodynamics&rft_subject=GEOPHYSICS&rft_subject=Expanding Knowledge in the Earth Sciences&rft_subject=EXPANDING KNOWLEDGE&rft_subject=EXPANDING KNOWLEDGE&rft_subject=Pure basic research&rft.type=dataset&rft.language=English Access the data

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This data collection is associated with the publication: Gibbons, A. D., Whittaker, J. M., & Müller, R. D. (2013). The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best-fit tectonic model. Journal of Geophysical Research: Solid Earth, 118(3), 808-822. doi: 10.1002/jgrb.50079

Publication Abstract

Published models for the Cretaceous seafloor-spreading history of East Gondwana result in unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate particular constraints from at least one of the associated ocean basins. We link East Gondwana spreading corridors by integrating magnetic and gravity anomaly data from the Enderby Basin off East Antarctica within a regional plate kinematic framework to identify a conjugate series of east-west-trending magnetic anomalies, M4 to M0 (~126.7–120.4 Ma). The mid-ocean ridge that separated Greater India from Australia-Antarctica propagated from north to south, starting at ~136Ma northwest of Australia, and reached the southern tip of India at ~126 Ma. Seafloor spreading in the Enderby Basin was abandoned at ~115 Ma, when a ridge jump transferred the Elan Bank and South Kerguelen Plateau to the Antarctic plate. Our revised plate kinematic model helps resolve the problem of successive two-way strike-slip motion between Madagascar and India seen in many previously published reconstructions and also suggests that seafloor spreading between them progressed from south to north from 94 to 84 Ma. This timing is essential for tectonic flow lines to match the curved fracture zones of the Wharton and Enderby basins, as Greater India gradually began to unzip from Madagascar from ~100 Ma. In our model, the 85-East Ridge and Kerguelen Fracture Zone formed as conjugate flanks of a “leaky” transform fault following the ~100Ma spreading reorganization. Our model also identifies the Afanasy Nikitin Seamounts as products of the Conrad Rise hotspot.

Authors and Institutions

Ana D. Gibbons - EarthByte Research Group, School of Geosciences, The University of Sydney, Australia

Joanne M. Whittaker - EarthByte Research Group, School of Geosciences, The University of Sydney, Australia. ORCID: 0000-0002-3170-3935

R. Dietmar Müller - EarthByte Research Group, School of Geosciences, The University of Sydney, Australia. ORCID: 0000-0002-3334-5764

Overview of Resources Contained

This data collection includes the all of the files needed to visualise, recreate, and interact with the plate motion model developed and published in Gibbons et al. (2013). Data used in the development of the plate motion model are also included.

List of Resources

Note: For details on the files included in this data collection, see “Description_of_Resources.txt”.

Note: For information on file formats and what programs to use to interact with various file formats, see “File_Formats_and_Recommended_Programs.txt”.

  • Rotation file for the tectonic model (.rot, 537 KB)
  • Continent-ocean boundary geometries (.gpml, .kml, .txt, .shp, total 684 KB)
  • Extinct ridge geometries (.gpml, .kml, .txt, .shp, total 414 KB)
  • Fracture zone geometries (.gpml, .kml, .txt, .shp, total 6.8 MB)
  • Isochron geometries (.gpml, .kml, .txt, .shp, total 4 MB)
  • Large igneous province outlines (.gpml, .kml, .txt, .shp, total 279 KB)
  • Magnetic anomaly picks (.gpmlz, .kml, .txt, .shp, total 17.5 MB)

For more information on this data collection, and links to other datasets from the EarthByte Research Group please visit EarthByte

For more information about using GPlates, including tutorials and a user manual please visit GPlates or EarthByte

Data time period: Jurassic to present day (~200–0 Ma)

This dataset is part of a larger collection

Click to explore relationships graph

-5.90272,-60.07405 -5.90272,30.43276 160.7379,30.43276 160.7379,-60.07405 -5.90272,-60.07405

77.417590273547,-14.82064125662

text: East Gondwana

text: Indian Ocean

text: Bounding Box: 30N, 6W; 60S, 6W; 60S, 160E; 30N, 160E

Identifiers