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pro vyhledávání: '"Gareth Hurman"'
Traditionally interpretations assume that as magma-rich rift settings mature, the magmatism accommodates greater amounts of extension at the expense of mechanical deformation. However, the importance of faulting in the final stages of magma-rich rift
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7763ac40c64a29ce32232599f6cc03f3
https://doi.org/10.5194/egusphere-egu23-14948
https://doi.org/10.5194/egusphere-egu23-14948
At mature magma-rich continental rifts, extension focuses along discrete axial segments where magmatism and diking are important in accommodating plate divergence. However, the role of magma in influencing the deformation at rift–rift offsets is st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b1849b6e57527950065c839939e6c36
https://eprints.soton.ac.uk/457954/
https://eprints.soton.ac.uk/457954/
Continental extension at mature rifts systems focuses along spreading segments where dominant magmatic activity, diking and minor faulting assist plate divergence. Such processes make adjacent spreading segments grow but also interact at zones where
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f646f86afb294e25cc7a24e0eebcfa98
https://doi.org/10.5194/egusphere-egu22-1175
https://doi.org/10.5194/egusphere-egu22-1175
Publikováno v:
Goldschmidt2022 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9d854866e599e25e19395b5b2e73b77
https://doi.org/10.46427/gold2022.9622
https://doi.org/10.46427/gold2022.9622
