Why intracontinental basins subside longer - 3D feedback effects of 
lithospheric cooling and sedimentation on the flexural strength of the 
lithosphere

Cacace, Mauro; Scheck-Wenderoth, Magdalena

doi:http://doi.org/10.2312/GFZ.LIS.2015.003

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Why intracontinental basins subside longer - 3D feedback effects of lithospheric cooling and sedimentation on the flexural strength of the lithosphere

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/persons/resource/cacace

Cacace, Mauro
6.1 Basin Modelling, 6.0 Geotechnologies, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/leni

Scheck-Wenderoth, Magdalena
6.1 Basin Modelling, 6.0 Geotechnologies, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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http://www.geoberlin2015.de/assets/book_of_abstracts_geoberlin_2015.pdf#section*.162
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Citation

Cacace, M., Scheck-Wenderoth, M. (2015): Why intracontinental basins subside longer - 3D feedback effects of lithospheric cooling and sedimentation on the flexural strength of the lithosphere, (Exkursionsführer und Veröffentlichungen der Deutschen Gesellschaft für Geowissenschaften ; 255), GeoBerlin (Berlin 2015), 108.
https://doi.org/http://doi.org/10.2312/GFZ.LIS.2015.003

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_1700901

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