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pro vyhledávání: '"Donna Shillington"'
Models of continental margins evolution are largely based on incomplete information, much of it built on research that is now >20 years old. Recent developments in parallel computing and novel geophysical approaches provide now the means to obtain a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd294c1a5e8fd2a55c9fe50b6514fed9
https://doi.org/10.5194/egusphere-egu23-9465
https://doi.org/10.5194/egusphere-egu23-9465
Autor:
Collin Brandl, Lindsay L. Worthington, Maria Beatrice Magnani, Donna Shillington, Thomas W Luckie
Detailed models of crustal structure at volcanic passive margins offer insight into the role of magmatism and distribution of igneous addition during continental rifting. The Eastern North American Margin (ENAM) is a volcanic passive margin that form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61d83d815fc8d3a52688e7c4a6f32da4
https://doi.org/10.22541/essoar.167689410.00443777/v1
https://doi.org/10.22541/essoar.167689410.00443777/v1
Autor:
Donna Shillington, James Gaherty, Christopher Scholz, Andrew Nyblade, Patrick Chindandali, Richard Wambura Ferdinand, Gabriel Mbogoni, Emily Hopper, Natalie Accardo, Gabrielle Tepp, Ashley Grivalja, David Borrego, Gabriel Mulibo
Few constraints are available on variations in extension with depth and along-strike in early stage continental rift systems, leaving many questions on the mechanisms of extension and the controlling factors. The Malawi (Nyasa) Rift in the southern E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::394fa08161e3ff5730c0f3a09d6e5604
https://doi.org/10.5194/egusphere-egu22-6839
https://doi.org/10.5194/egusphere-egu22-6839