Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Reidar G. Trønnes"'
Autor:
Grace E. Shephard, Christine Houser, John W. Hernlund, Juan J. Valencia-Cardona, Reidar G. Trønnes, Renata M. Wentzcovitch
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
This study identifies the predicted seismic expression of the high-to-low iron spin crossover in the deep Earth mineral ferropericlase. A depth-dependent signal is detected in the fastest and slowest regions, related to lateral temperature variations
Externí odkaz:
https://doaj.org/article/6e36326334c346a180cffbc204e410e9
Publikováno v:
American Mineralogist. 105:1014-1020
The subsolidus phase diagram of silica in the 80–220 GPa pressure range was determined by density functional theory (DFT). The transition pressures calculated using the generalized gradient approximation (GGA) in the static limit (at 0 K, without z
Autor:
John Hernlund, Reidar G. Trønnes, Christine Houser, Grace E. Shephard, Juan Valencia-Cardona, Renata M. Wentzcovitch
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Nature Communications
Nature Communications
The two most abundant minerals in the Earth’s lower mantle are bridgmanite and ferropericlase. The bulk modulus of ferropericlase (Fp) softens as iron d-electrons transition from a high-spin to low-spin state, affecting the seismic compressional ve
Earth's heat budget is strongly influenced by spatial and temporal variations in surface heat flow caused by plate tectonic cycles. Here, we use a novel set of paleo‐seafloor age grids extending back to the mid‐Paleozoic to infer spatiotemporal v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fb6e1e6f51376f382106ea499e03c292
http://hdl.handle.net/10852/85815
http://hdl.handle.net/10852/85815
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Deep-rooted mantle plumes are thought to originate from the margins of the Large Low Shear Velocity Provinces (LLSVPs) at the base of the mantle. Visible in seismic tomography, the LLSVPs are usually interpreted to be intrinsically dense thermochemic
The lower mantle can be grouped into high, low, and average (i.e., ambient) seismic velocity domains at each depth, based on the amplitude and polarity of wavespeed perturbations (% δlnVs, % δlnVp). Many studies focus on elucidating the thermo-chem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4013b9cfc4df458ab05984ac9215e98e
https://doi.org/10.5194/egusphere-egu2020-11806
https://doi.org/10.5194/egusphere-egu2020-11806
Deep-rooted mantle plumes are thought to originate from the margins of the Large Low Shear Velocity Provinces (LLSVPs) at the base of the mantle. Visible in seismic tomography, the LLSVPs are often numerically modeled as dense and viscous thermochemi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::611ad63d58a29d65e021d9f61a586f89
https://doi.org/10.5194/egusphere-egu2020-5577
https://doi.org/10.5194/egusphere-egu2020-5577
Publikováno v:
Geophysical Research Letters. 45:7523-7532
The large low shear velocity provinces (LLSVPs) observed in the lowermost mantle are widely accepted as chemically distinct thermochemical 'piles', but their origin and long-term evolution remain poorly understood. The survival time and shape of the
Autor:
Weiwei Wang, Michael J. Walter, M. A. Baron, Reidar G. Trønnes, Robert Myhill, Oliver T. Lord, Andrew Thomson
Publikováno v:
Baron, M A, Lord, O T, Myhill, R, Thomson, A R, Wang, W, Trønnes, R G & Walter, M J 2017, ' Experimental constraints on melting temperatures in the MgO–SiO2 system at lower mantle pressures ', Earth and Planetary Science Letters, vol. 472, pp. 186-196 . https://doi.org/10.1016/j.epsl.2017.05.020
Eutectic melting curves in the system MgO–SiO2 have been experimentally determined at lower mantle pressures using laser-heated diamond anvil cell (LH-DAC) techniques. We investigated eutectic melting of bridgmanite plus periclase in the MgO–MgSi
Autor:
Ludovic Ferrière, Reidar G. Trønnes, Richard Wirth, Mariana Klementová, A. Greshake, Lukáš Palatinus, Ute Böttger, Vera A. Fernandes, Jörg Fritz
Publikováno v:
American Mineralogist
Fritz, J, Greshake, A, Klementova, M, Wirth, R, Palatinus, L, Trønnes, R G, A. Fernandes, V, Böttger, U & Ferrière, L 2020, ' Donwilhelmsite, [CaAl4Si2O11], a new lunar high-pressure Ca-Al-silicate with relevance for subducted terrestrial sediments ', American Mineralogist . https://doi.org/10.2138/am-2020-7393
Fritz, J, Greshake, A, Klementova, M, Wirth, R, Palatinus, L, Trønnes, R G, A. Fernandes, V, Böttger, U & Ferrière, L 2020, ' Donwilhelmsite, [CaAl4Si2O11], a new lunar high-pressure Ca-Al-silicate with relevance for subducted terrestrial sediments ', American Mineralogist . https://doi.org/10.2138/am-2020-7393
We report on the occurrence of a new high-pressure Ca-Al-silicate in localized shock melt pockets found in the feldspatic lunar meteorite Oued Awlitis 001 and discuss the implications of our discovery. The new mineral crystallized as tiny, micrometer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0392e6e94524dbb2aa0f81b325a79502
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5004273
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5004273