Zobrazeno 1 - 10
of 79
pro vyhledávání: '"E. Hooft"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 7, Pp n/a-n/a (2022)
Abstract The Kolumbo submarine volcano in the southern Aegean (Greece) is associated with repeated seismic unrest since at least two decades and the causes of this unrest are poorly understood. We present a ten‐month long microseismicity data set f
Externí odkaz:
https://doaj.org/article/18f03f0bfee94254a791d284cec29c8d
Publikováno v:
Nature Geoscience. 16:446-453
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19edb017947a8814f687f608e9e7609f
https://doi.org/10.1038/s41561-023-01160-z
https://doi.org/10.1038/s41561-023-01160-z
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 12, Pp n/a-n/a (2020)
Abstract Recent seismic results from the Cascadia Initiative indicate that heterogeneity in the oceanic asthenosphere affects subduction dynamics. Accurate characterization of the oceanic upper mantle is thus necessary to fully understand subduction
Externí odkaz:
https://doaj.org/article/13f7604a66ea415f8e09653fe999ceb8
Autor:
Jens Karstens, Jonas Preine, Gareth J. Crutchley, Steffen Kutterolf, Willem G. M. van der Bilt, Emilie E. E. Hooft, Timothy H. Druitt, Florian Schmid, Jan Magne Cederstrøm, Christian Hübscher, Paraskevi Nomikou, Steven Carey, Michel Kühn, Judith Elger, Christian Berndt
Publikováno v:
Nature Communications
Despite their global societal importance, the volumes of large-scale volcanic eruptions remain poorly constrained. Here, we integrate seismic reflection and P-wave tomography datasets with computed tomography-derived sedimentological analyses to esti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::322c4ecd7d01b559646f42ae1fa4e96a
https://hdl.handle.net/11250/3067777
https://hdl.handle.net/11250/3067777
Autor:
K. Chrapkiewicz, M. Paulatto, B. A. Heath, E. E. E. Hooft, P. Nomikou, C. B. Papazachos, F. Schmid, D. R. Toomey, M. R. Warner, J. V. Morgan
Publikováno v:
Geochemistry, Geophysics, Geosystems. 23
Arc volcanoes are underlain by complex systems of molten-rock reservoirs ranging from melt-poor mush zones to melt-rich magma chambers. Petrological and satellite data indicate that eruptible magma chambers form in the topmost few kilometres of the c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a3090fffb9397cfacbc853960f08ec14
https://doi.org/10.1029/2022gc010475
https://doi.org/10.1029/2022gc010475
Publikováno v:
Journal of Maps, Vol 17, Iss 3, Pp 111-121 (2021)
Geologic maps are foundational products for natural hazard assessments but developing them for submarine areas is challenging due to a lack of physical access to the study area. In response, submarine geomorphologic maps are used to provide geologic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0ba7dcf24db602c092c3c85a30f08ee6
https://doaj.org/article/78c9281cfa4a456882034fbf50af7cf3
https://doaj.org/article/78c9281cfa4a456882034fbf50af7cf3
Autor:
Konstantina Bejelou, Emilie E. E. Hooft, Demitris Paradissis, Paraskevi Nomikou, Konstantinos Raptakis, Melissinos Paraskevas
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 51, Iss 1, Pp 1-24 (2021)
Santorini is located in the central part of the Hellenic Volcanic Arc (South Aegean Sea) and is well known for the Late-Bronze-Age “Minoan” eruption that may have been responsible for the decline of the great Minoan civilization on the island of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a18954f4b435e823e21cc091f72013e8
https://doi.org/10.31577/congeo.2021.51.1.1
https://doi.org/10.31577/congeo.2021.51.1.1
Autor:
Joanna Morgan, Emilie E. E. Hooft, B. A. Heath, C. B. Papazachos, Douglas R. Toomey, Michele Paulatto, Paraskevi Nomikou, Brennah McVey
Publikováno v:
Geology. 48:231-235
Despite multidisciplinary evidence for crustal magma accumulation below Santorini volcano, Greece, the structure and melt content of the shallow magmatic system remain poorly constrained. We use three-dimensional (3-D) velocity models from tomographi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0f8f2d1947809390f91d1e2d030f98e
https://doi.org/10.1130/g47127.1
https://doi.org/10.1130/g47127.1
Autor:
Douglas R. Toomey, C. B. Papazachos, Paraskevi Nomikou, Joanna Morgan, B. A. Heath, Michele Paulatto, Emilie E. E. Hooft
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6278d7363dcfb59a3f837a7526cc82e8
https://doi.org/10.1029/2021jb021898
https://doi.org/10.1029/2021jb021898
Autor:
B. A. Heath, Emilie E. E. Hooft, Douglas R. Toomey, Michael Warner, C. B. Papazachos, Joanna Morgan, Michele Paulatto, Paraskevi Nomikou
Publikováno v:
Journal of Geophysical Research: Solid Earth
At extensional volcanic arcs, faulting often acts to localize magmatism. Santorini is located on the extended continental crust of the Aegean microplate and is one of the most active volcanoes of the Hellenic arc, but the relationship between tectoni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b40f14d61c3a21f1cb99057ae17b32c9
https://doi.org/10.1029/2019jb017699
https://doi.org/10.1029/2019jb017699