Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Froukje M. van der Zwan"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-7 (2024)
Abstract Mantle plumes are responsible for the Earth’s largest volcanic provinces. In the prevailing paradigm, the deep mantle is less degassed than convecting shallow mantle, implying that plume-derived lavas have higher concentrations of primordi
Externí odkaz:
https://doaj.org/article/04f0934100a144e78b662e5a66caee0a
Autor:
Froukje M. van der Zwan, Nico Augustin, Sven Petersen, Sharifah M. Altalhi, Júnia Schultz, Raquel S. Peixoto, Jörg Follmann, Arthur Anker, Francesca Benzoni, Evelyn R. Garcia Paredes, Murtadha Al Malallah, Lera Shepard, Mustapha Ouhssain, S. Beatrice Jägerup, Burton H. Jones, Alexandre S. Rosado
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-13 (2023)
Abstract For decades, hydrothermal activity along the Red Sea Rift was only inferred from metalliferous sediments and hot brines. Active hydrothermal fluid discharge was never directly observed from this young ocean basin, but could be key to underst
Externí odkaz:
https://doaj.org/article/d5553789deeb41a895c256030470926e
Autor:
Laura Macrina, Megan K. B. Nolan, Tullia I. Terraneo, Nicolas Oury, Nico Augustin, Froukje M. van der Zwan, Francesca Benzoni
Publikováno v:
Frontiers in Marine Science, Vol 10 (2024)
Octocorals (Cnidaria: Anthozoa) have a global distribution and form benthic assemblages along the depth gradient, from shallow to deep waters. They often occur below SCUBA diving limits, where they can become dominant habitat builders and aggregate d
Externí odkaz:
https://doaj.org/article/1d1753c80d604e80a63816fcd9f65fed
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
The mid-ocean rift in the Red Sea is one of the youngest rifting systems on Earth. Only recently, state-of-the-art methods and modern deep-sea instruments have been used to explore this young and unique volcanic system. During the first autonomous un
Externí odkaz:
https://doaj.org/article/cc7f1b847f19454b859322cf835e165a
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-10 (2021)
Here, based on earthquake data, vertical gravity gradient data and high-resolution bathymetry, the authors show that the Red Sea is not in transition from rifting to spreading as previously proposed. They instead suggest it to be a mature ocean basin
Externí odkaz:
https://doaj.org/article/b09fac9a66ac4b94a72a035d689a8cfc
Autor:
Jörg Follmann, Froukje M. van der Zwan, Jonas Preine, Christian Hübscher, Romain Bousquet, Nico Augustin
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Plutonic rocks such as gabbros provide information on magmatic and tectonic processes which occur beneath a mid-ocean rift axis as well as on the formation of the oceanic crust. Igneous rocks, reported from the Red Sea Rift valley, have been limited
Externí odkaz:
https://doaj.org/article/87a328704d8c4477a3f44a310f577b3a
The mid-ocean rift in the Red Sea is recently regaining attention in the geosciences due to the possibility of investigating this young ocean in more detail than ever by state-of-the-art methods and modern deep-sea instrumentation. During the first A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7104d1d1d53c9d820dd8f996eca14b69
https://doi.org/10.5194/egusphere-egu23-13869
https://doi.org/10.5194/egusphere-egu23-13869
Autor:
Margherita Fittipaldi, Daniele Trippanera, Nico Augustin, Froukje M. van der Zwan, Alexander Petrovic, Dirk Metz, Sigurjon Jónsson
The Red Sea is a unique place to study a young oceanic rift basin and the interplay between magma and tectonics at a young divergent plate boundary. The spreading rate of the Red Sea rift changes from ~17 mm/yr in the south to ~7 mm/yr in the north,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4fc729a86ca9706fe08a5239c29cef84
https://doi.org/10.5194/egusphere-egu22-11791
https://doi.org/10.5194/egusphere-egu22-11791
Basalts from high flux intra-plate volcanism (Iceland, Hawaii, Samoa) are characterised by 3He/4He that are significantly higher than those from the upper mantle sampled at mid-ocean ridges. The prevailing paradigm requires that a largely undegassed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c39b05cc24e014d4abb100215231ba9d
https://doi.org/10.5194/egusphere-egu22-4994
https://doi.org/10.5194/egusphere-egu22-4994
Autor:
Nico Augustin, Christian Hübscher, Froukje M. van der Zwan, Romain Bousquet, Jörg Follmann, Jonas Preine
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Plutonic rocks such as gabbros provide information on magmatic and tectonic processes which occur beneath a mid-ocean rift axis as well as on the formation of the oceanic crust. Igneous rocks, reported from the Red Sea Rift valley, have been limited
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::77db55ddbea3bb995113f1a83c592c35
https://doi.org/10.3389/feart.2021.742815
https://doi.org/10.3389/feart.2021.742815