A Reply to the Comment on “Assessing Discrepancies Between Previous Plate Kinematic Models of Mesozoic Iberia and Their Constraints” by Barnett-Moore Et Al.
Author:
Affiliation:
1. Currently unemployed
2. Instituto Dom Luiz, Faculdade de Ciências; Universidade de Lisboa; Lisbon Portugal
3. Instituto Português do Mar e da Atmosfera; Lisbon Portugal
Funder
Portuguese National Science Foundation
Fundação para a Ciência e a Tecnologia
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017TC004760/fullpdf
Reference64 articles.
1. Dynamic topography and eustasy controlled the paleogeographic evolution of northern Africa since the mid Cretaceous;Barnett-Moore;Tectonics,2017
2. Assessing discrepancies between previous plate kinematic models of Mesozoic Iberia and their constraints;Barnett-Moore;Tectonics,2016
3. Magmatic breakup as an explanation for magnetic anomalies at magma-poor rifted margins;Bronner;Nature Geoscience,2011
4. Refining the Early Devonian time scale using Milankovitch cyclicity in Lochkovian-Pragian sediments (Prague Synform, Czech Republic);Da Silva;Earth and Planetary Science Letters,2016
5. Geomagnetic secular variation and the statistics of palaeomagnetic directions;Deenen;Geophysical Journal International,2011
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