Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Valera P. Shcherbakov"'
Autor:
Karl Fabian, Valera P. Shcherbakov
Publikováno v:
Geophysical Journal International. 221:2104-2112
SUMMARY The natural remanent magnetization (NRM) of the ocean floor is carried by titanomagnetite grains that undergo low-temperature oxidation after initial cooling. Progressing oxidation is known to generate shrinkage cracks in grains larger than a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8395dc3cdc4bbe039bf423537e30beb
https://doi.org/10.1093/gji/ggaa142
https://doi.org/10.1093/gji/ggaa142
Autor:
Andrew J. Biggin, Valera P. Shcherbakov, V. V. Shcherbakova, Daniele Thallner, Vladimir Bakhmutov, G. V. Zhidkov
Publikováno v:
GEOPHYSICAL JOURNAL INTERNATIONAL
SUMMARY The time-averaged geomagnetic field is generally purported to be uniformitarian across Earth history—close to a geocentric axial dipole, with average strength within one order of magnitude of that at present. Nevertheless, recent studies ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::26a23aa1adf1f483199c4c2e43c7e29e
https://doi.org/10.1093/gji/ggz566
https://doi.org/10.1093/gji/ggz566
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:7616-7632
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32379c1c9a1b5d0e990111e811c46bb1
https://doi.org/10.1029/2019jb017873
https://doi.org/10.1029/2019jb017873
Autor:
Karl Fabian, Valera P. Shcherbakov
The NRM of the ocean floor is carried by titanomagnetite grains that undergo low-temperature oxidation after initial cooling. Progressing oxidation is known to generate shrinkage cracks in grains larger than approximately 5 mkm, and is suspected to c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a2d759d760339908699680645871468
https://doi.org/10.5194/egusphere-egu2020-3733
https://doi.org/10.5194/egusphere-egu2020-3733
Autor:
Tiziana Boffa Ballaran, Karl Fabian, Richard J. Harrison, Suzanne A. McEnroe, Chris I. Thomas, Nobuyoshi Miyajima, Valera P. Shcherbakov, Benjamin P. Burton, Helmer Fjellvåg
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1fe1ce356b29119c0cf54de7deedf9f
https://doi.org/10.1130/abs/2020am-357624
https://doi.org/10.1130/abs/2020am-357624
Publikováno v:
Izvestiya, Physics of the Solid Earth. 53:714-732
The results of paleomagnetic studies and paleointensity determinations from two Neoarchaean Shala dikes with an age of ~2504 Ma, located within the Vodlozerskii terrane of the Karelian craton, are presented. The characteristic components of primary m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03017c9e503970d6872fc855e6a91752
https://doi.org/10.1134/s1069351317050111
https://doi.org/10.1134/s1069351317050111
Publikováno v:
Russian Geology and Geophysics. 58:1118-1128
Many Permian–Triassic dolerite samples from the Siberian Trap Large Igneous Province exposed to conventional stepwise thermal demagnetization at 250–450 °C display mid-temperature remanence (MTC) directed opposite to the high-temperature NRM com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad382a1ba07a54ccb06ab4419760ae94
https://doi.org/10.1016/j.rgg.2017.08.008
https://doi.org/10.1016/j.rgg.2017.08.008
Autor:
Nikolai Petersen, Valera P. Shcherbakov, Gwenaël Hervé, S. Ostner, V. V. Shcherbakova, Florian Lhuillier
Publikováno v:
Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2019, 216 (2), pp.1482-1494. ⟨10.1093/gji/ggy491⟩
Geophysical Journal International, 2019, 216 (2), pp.1482-1494. ⟨10.1093/gji/ggy491⟩
Geophysical Journal International, Oxford University Press (OUP), 2019, 216 (2), pp.1482-1494. ⟨10.1093/gji/ggy491⟩
Geophysical Journal International, 2019, 216 (2), pp.1482-1494. ⟨10.1093/gji/ggy491⟩
International audience; We conducted an absolute palaeointensity (API) survey on Ethiopian volcanics from Early Oligocene (Belessa section) and Middle Miocene (Debre Sina section). After a careful selection based on the reversibility of high-field th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::91944dce8b67459b25a01459008c9d65
https://hal.inrae.fr/hal-02622551
https://hal.inrae.fr/hal-02622551
Publikováno v:
Springer Geophysics ISBN: 9783319904368
Laboratory modeling of the CRM formation on basaltic rocks from the Reykjanes submarine ridge and the Red Sea rift zone containing titanomagnetites (TM) with Tc ≈ 200 °C was carried out by annealing at different temperatures Tan for different time
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64a99eac0fd9534962e75dbc105ecd4e
https://doi.org/10.1007/978-3-319-90437-5_14
https://doi.org/10.1007/978-3-319-90437-5_14
Autor:
Karl Fabian, Valera P. Shcherbakov
This article has been accepted for publication in Geophysical Journal International © 2018. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved. Source at https://doi.org/10.1093/gji/ggy285. A first-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df69f0bee54438c1afba6fb05e38949b
https://hdl.handle.net/10037/13626
https://hdl.handle.net/10037/13626