Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Thomas Duvernay"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 2, Pp n/a-n/a (2024)
Abstract Owing to their abundance and relative availability on Earth's seafloor, mid‐ocean ridge basalts (MORBs) have a well‐defined chemical element budget, reflected by the low standard deviation associated with typical normal MORB (N‐MORB) c
Externí odkaz:
https://doaj.org/article/6fac2b00e15445acb0ec70254e1b3ecf
Autor:
Thomas Duvernay, D. Rhodri Davies, Christopher R. Mathews, Angus H. Gibson, Stephan C. Kramer
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 7, Pp n/a-n/a (2022)
Abstract Several of Earth's intra‐plate volcanic provinces lie on or adjacent to continental lithosphere. Although many are believed to mark the surface expression of mantle plumes, our limited understanding of how buoyant plumes interact with hete
Externí odkaz:
https://doaj.org/article/2b760363755d499791775cb7e9113bee
Autor:
Thomas Duvernay, D. Rhodri Davies, Christopher R. Mathews, Angus H. Gibson, Stephan C. Kramer
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract Several of Earth's intraplate volcanic provinces are hard to reconcile with the mantle plume hypothesis. Instead, they exhibit characteristics that are more compatible with shallower processes that involve the interplay between uppermost man
Externí odkaz:
https://doaj.org/article/d1d496c1a8254857b513ae8fad357d7b
Autor:
Thomas Duvernay
In 1871, five ships of the United States Asiatic Fleet headed into Korean waters, intent on establishing relations with Korea, a country that had shunned the outside world for centuries. However, as the country had been in conflict with Western count
Autor:
Thomas Duvernay, Rhodri Davies
Volcanic provinces within Earth's continents exhibit a wide range of characteristics that reflect the intricate nature of the dynamic interactions at their origin. To improve our understanding of the driving mechanisms at play, we address the generat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9ad7dc4474b07a07552a3add3e9f79a
https://doi.org/10.5194/egusphere-egu23-10559
https://doi.org/10.5194/egusphere-egu23-10559
Publikováno v:
Geochemistry, Geophysics, Geosystems. 23
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f474887eab0ea7c23acf855415e89f8f
https://doi.org/10.1029/2022gc010363
https://doi.org/10.1029/2022gc010363
Geodynamical simulations underpin our understanding of upper-mantle processes, but their predictions require validation against observational data. Widely used geophysical datasets provide limited ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61e89ecb497200e564cb88e575a9919e
https://doi.org/10.1002/essoar.10507843.1
https://doi.org/10.1002/essoar.10507843.1
Publikováno v:
Geochemistry, Geophysics, Geosystems. 22
Several of Earth's intra-plate volcanic provinces are hard to reconcile with the mantle plume hypothesis. Instead, they exhibit characteristics that are more compatible with shallower processes tha...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd46e718f22a2152d5426e2ca25997e1
https://doi.org/10.1029/2021gc009953
https://doi.org/10.1029/2021gc009953
Several of Earth's intra-plate volcanic provinces cannot be explained solely through the classical mantle plume hypothesis. Instead, they are believed to be generated by shallower processes that involve the interplay between uppermost mantle flow and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::93350b097d9c0d6771759a91bfd2beba
https://doi.org/10.5194/egusphere-egu21-1023
https://doi.org/10.5194/egusphere-egu21-1023