Extensional Polarity Change in Continental Rifts: Inferences From 3-D Numerical Modeling and Observations

Author:

Balázs A.12ORCID,Matenco L.1ORCID,Vogt K.3,Cloetingh S.1,Gerya T.4

Affiliation:

1. Tectonics Group, Department of Earth Sciences, Faculty of Geosciences; Utrecht University; Utrecht Netherlands

2. Now at Laboratory of Experimental Tectonics, Department of Sciences; Università degli Studi Roma Tre; Rome Italy

3. International Geothermal Centre; Bochum University of Applied Sciences; Bochum Germany

4. Geophysical Fluid Dynamics Group; Institute of Geophysics, ETH; Zurich Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference78 articles.

1. Factors controlling the mode of rift interaction in brittle-ductile coupled systems: A 3D numerical study;Allken;Geochemistry, Geophysics, Geosystems,2012

2. Rift-shear architecture and tectonic development of the Ghana margin deduced from multichannel seismic reflection and potential field data;Antobreh;Marine and Petroleum Geology,2009

3. Symmetry during the syn- and post-rift evolution of extensional back-arc basins: The role of inherited orogenic structures, Earth planet;Balázs;Science Letters,2017

4. The link between tectonics and sedimentation in back-arc basins: New genetic constraints from the analysis of the Pannonian Basin;Balázs;Tectonics,2016

5. Factors controlling the Alpine evolution of Central Pyrenees inferred from the comparison of observations and geodynamical models;Beaumont;Journal of Geophysical Research,2000

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