AcknowledgmentsThe authors would like to thank the full SEISMIX 2016 organization team and participants for facilitating and taking part in the experiment in Aviemore (Scotland). ION is thanked for supplying the seismic profile used in the experiments. Dr. Eagles and Dr. Pérez-Díaz are thanked for kindly sharing the interpretations of the E-India margin. JA is funded by “Juan de la Cierva-Incorporación” fellow-ship IJC2018-036074-I and “Ramón y Cajal” fellowship RYC2021-033872-I, funded by MCIN/AEI/https://doi.org/10.13039/501100011033 and the European Union NextGenerationEU/PRTR. We thank the reviewers for their constructive comments, and Jonathan Aitchison for the editorial guidance.Peer reviewedPostprintPublisher PD
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International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
19th International Symposium on Deep Seismic Profiling of the Continents and their Margins (SEISMIX ...
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The causes of continental breakup are still poorly understood. More and more it becomes evident that...
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International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
The idea of a simple linear boundary between continental and oceanic crust at extended continental m...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
19th International Symposium on Deep Seismic Profiling of the Continents and their Margins (SEISMIX ...
X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizPara entender el estado actual y la...
Oil and gas exploration uses accurate interpretations of the sedimentary basins that populate the co...
Wide-angle seismic Passive margins We have performed a global study of 2D crustal scale wide-angle p...
The Murray Ridge/Dalrymple Trough system forms the boundary between the Indian and Arabian plates i...
The presence of SDRs (seawrd dipping reflectors) on the regional lines around the Indian continent ...
Abstract: The segmented East Indian continental margin developed after the Early Cretaceous break-up...
The causes of continental breakup are still poorly understood. More and more it becomes evident that...
The lithospheric architecture of passive margins is crucial for understanding the tectonic processes...
Magma-poor rift margins provide the ideal environment in which to study the processes responsible fo...
The crustal structure of the Mesozoic deep Galicia margin and adjacent ocean-continent boundary (OCB...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
The idea of a simple linear boundary between continental and oceanic crust at extended continental m...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...
International audienceWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping...