Data for: Similar Crust beneath Disrupted and Intact Cratons: Arguments Against Lower-crust Delamination as A Decratonization Trigger

Published: 17 Nov 2018 | Version 1 | DOI: 10.17632/fhscpnxrc2.1
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Description of this data

Thickness, observed and corrected P-wave velocity and estimated compositions of the crust of the Wendeng-Alashan transect (Line 41) in the North China Craton.

Experiment data files

This data is associated with the following publication:

Similar crust beneath disrupted and intact cratons: Arguments against lower-crust delamination as a decratonization trigger

Published in: Tectonophysics

Latest version

  • Version 1

    2018-11-17

    Published: 2018-11-17

    DOI: 10.17632/fhscpnxrc2.1

    Cite this dataset

    Ma, Qiang (2018), “Data for: Similar Crust beneath Disrupted and Intact Cratons: Arguments Against Lower-crust Delamination as A Decratonization Trigger”, Mendeley Data, v1 http://dx.doi.org/10.17632/fhscpnxrc2.1

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Geochemistry, Geophysics

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The files associated with this dataset are licensed under a Attribution-NonCommercial 3.0 Unported licence.

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You are free to adapt, copy or redistribute the material, providing you attribute appropriately and do not use the material for commercial purposes.

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