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Rift migration explains continental margin asymmetry and crustal hyper-extension

When continents break apart, continental crust and lithosphere are thinned until break-up is achieved and an oceanic basin is formed. The most remarkable and least understood structures associated with this process are up to 200 km wide areas of hyper-extended continental crust, which are partitione...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Brune, Sascha, Heine, Christian, Pérez-Gussinyé, Marta, Sobolev, Stephan V.
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Nature Pub. Group 2014
Gaiak:
Sarrera elektronikoa:https://ncbi.nlm.nih.gov/pmc/articles/PMC4059923/
https://ncbi.nlm.nih.gov/pubmed/24905463
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms5014
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